tag:blogger.com,1999:blog-92069193997647017122024-02-20T17:25:41.464+01:00Pedogeographia ComenianaThis blog is edited by Peter Pišút, Comenius University, Faculty of Natural Sciences, Department of Physical Geography and Geoecology, Mlynská dolina, 842 15, Bratislava 4, SlovakiaUnknownnoreply@blogger.comBlogger309125tag:blogger.com,1999:blog-9206919399764701712.post-10210444844082887832012-11-02T12:15:00.007+01:002012-11-02T12:53:42.015+01:00Kambizem pseudoglejová, kyslá<div class="separator" style="clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgMDQ2mB39GjOzMmd72MUTCXBNVhHbPwIf4CCiamhUMWkP6PWPR4t6AllMWD7d3Wsax98qbCnK8_8KCD3TiXOAUD8c9K2ZOxYs2TNnbvOZQODiGIm0lGrPtzy0wVo19hJyOz375bRw-054/s1600/IMG_3587.jpg" imageanchor="1" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img border="0" height="200" qea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgMDQ2mB39GjOzMmd72MUTCXBNVhHbPwIf4CCiamhUMWkP6PWPR4t6AllMWD7d3Wsax98qbCnK8_8KCD3TiXOAUD8c9K2ZOxYs2TNnbvOZQODiGIm0lGrPtzy0wVo19hJyOz375bRw-054/s200/IMG_3587.jpg" width="150" /></a><span style="font-family: "Trebuchet MS", sans-serif;">Location: Malé Karpaty Mts., Slovakia</span></div>
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<span style="font-family: "Trebuchet MS", sans-serif;">Site: Limbach, Tri Kamenné kopce / Nad Šenkárkou</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Elevation: 550 m a. s. l.</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Author of the photographies: P. Pišút ©, 30.3.2011</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Land use: commercial forest</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Vegetation: European beech wood (<em>Fagetum nudum</em>)</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification MKSP (2000): <a href="http://pedogeografiauk.blogspot.sk/2009/07/kambizem-pseudoglejova-kmg.html">Kambizem pseudoglejová, kyslá</a></span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification WRB (2006): Endogleyic Cambisol, dystric</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Parent rock: Weathering products of granitic rocks </span><br />
<span style="font-family: Verdana, sans-serif; font-size: x-small;">Remarks: Cambic horizon; gleyic colour pattern in the subsoil; krotovina</span><br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhXTYyep-QJLc94scXyNRtV2pOVblVQl-62LiMj2rfuQjaiZSi0JnZDFnZNaj-Oy2MimqJJrjixWtgPhs09GsnrkmKxrumJ5nltEJooh86Hrq2VkmsjL_aI5t2fTHuRuMhrae8H06HxiMI/s1600/IMG_3570.jpg" imageanchor="1" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img border="0" height="177" qea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhXTYyep-QJLc94scXyNRtV2pOVblVQl-62LiMj2rfuQjaiZSi0JnZDFnZNaj-Oy2MimqJJrjixWtgPhs09GsnrkmKxrumJ5nltEJooh86Hrq2VkmsjL_aI5t2fTHuRuMhrae8H06HxiMI/s200/IMG_3570.jpg" width="200" /></a></div>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh19EzYKokW655WlJskrMWoIvF6NHSapkRvWnf9QJklA630gcaJwf1YbRxUn6g2lKXTk4PQtgwVD2cYmS7Yxc0P2TUOUHDSTJT2W9dv2HWWDzjUdPH9_aejVd02uiVldKyS90vLDCwQe60/s1600/IMG_3593.jpg" imageanchor="1" style="clear: left; cssfloat: left; margin-bottom: 1em; margin-left: auto; margin-right: auto;"><img border="0" height="130" qea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh19EzYKokW655WlJskrMWoIvF6NHSapkRvWnf9QJklA630gcaJwf1YbRxUn6g2lKXTk4PQtgwVD2cYmS7Yxc0P2TUOUHDSTJT2W9dv2HWWDzjUdPH9_aejVd02uiVldKyS90vLDCwQe60/s200/IMG_3593.jpg" width="200" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-family: Times, "Times New Roman", serif; font-size: small;">Larger skelet clasts</span></td></tr>
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<table cellpadding="0" cellspacing="0" class="tr-caption-container" style="float: left; margin-right: 1em; text-align: left;"><tbody>
<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhCYgZjFo32fvhGaHTM1EhNBnlPgpyxDuKqkXqVxIYsxG-WhIMdY63HNEOodRl_MogllIE_0PA8hFX1BBjePUJkJKYBoqishBVM8bu6LYTe02rg1l9RE3IRdBYV-PkxEL8G3chTHcCowo0/s1600/IMG_3564.jpg" imageanchor="1" style="clear: left; cssfloat: left; margin-bottom: 1em; margin-left: auto; margin-right: auto;"><img border="0" height="150" qea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhCYgZjFo32fvhGaHTM1EhNBnlPgpyxDuKqkXqVxIYsxG-WhIMdY63HNEOodRl_MogllIE_0PA8hFX1BBjePUJkJKYBoqishBVM8bu6LYTe02rg1l9RE3IRdBYV-PkxEL8G3chTHcCowo0/s200/IMG_3564.jpg" width="200" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-family: Times, "Times New Roman", serif; font-size: small;">Gleyic colour pattern</span></td></tr>
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Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-36085597346208809002012-10-31T16:53:00.003+01:002012-10-31T17:13:18.487+01:00Kambizem modálna, Havešová<div class="separator" style="border-bottom: medium none; border-left: medium none; border-right: medium none; border-top: medium none; clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhI7qmiW0G8693L6OgD_d6ofYjxG_we8mfV1h9O1AM95cUbMue_qlfBFB1UiaR5fG79Jd9S_WWNgmkSNKFqhMzU5d4QUBk-QO_n3lXKIwA42rjgZTshLFyFbK30h6JezzQYWpffQwKdaEM/s1600/IMG_0017.JPG" imageanchor="1" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img border="0" height="200" qea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhI7qmiW0G8693L6OgD_d6ofYjxG_we8mfV1h9O1AM95cUbMue_qlfBFB1UiaR5fG79Jd9S_WWNgmkSNKFqhMzU5d4QUBk-QO_n3lXKIwA42rjgZTshLFyFbK30h6JezzQYWpffQwKdaEM/s200/IMG_0017.JPG" width="166" /></a></div>
<span style="font-family: "Trebuchet MS", sans-serif;">Location: Bukovské vrchy Mts., Slovakia</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Site: Havešová, Nastaz range</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Elevation: 597 m a. s. l.</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Author of the photographies: P. Pišút ©, 11.10.2012</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Land use: Nature Reserve</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Vegetation: European beech Carpathians primeval forest</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification MKSP (2000): <a href="http://pedogeografiauk.blogspot.sk/2008/07/kambizem-modlna-kmm.html">Kambizem modálna</a></span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification WRB (2006): Cambisol</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Parent rock: Weathering products of claystones and sandstones (flysch belt)</span><br />
<span style="font-family: Times, "Times New Roman", serif;">Note: Soil profile opened on the occassion of the pedological conference in Snina "Pedologické dni 2012".</span><br />
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<table cellpadding="0" cellspacing="0" class="tr-caption-container" style="float: left; margin-right: 1em; text-align: left;"><tbody>
<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj62APAS97zZcFm6Jrd-DOr5aydwkXoNgSImxT4sPo0Z3uIDMvauKPpv7hXGIvt8zeWfNSo2ZkGBhbNbJEDFQyGRsoUUQAu1XTKSiv7XABS9d9Ch3C4c4XgKP1WQH_TuSlrCyFBZynn-Xg/s1600/IMG_0022.JPG" imageanchor="1" style="clear: left; cssfloat: left; margin-bottom: 1em; margin-left: auto; margin-right: auto;"><img border="0" height="150" qea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj62APAS97zZcFm6Jrd-DOr5aydwkXoNgSImxT4sPo0Z3uIDMvauKPpv7hXGIvt8zeWfNSo2ZkGBhbNbJEDFQyGRsoUUQAu1XTKSiv7XABS9d9Ch3C4c4XgKP1WQH_TuSlrCyFBZynn-Xg/s200/IMG_0022.JPG" width="200" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;">Beech regrowth</td></tr>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiJeTXvB4UKUguL6f3ZjU8_JdJeh04cPOfYfWEZhjLg4G6PNeRxVuqWn_3RpeACWXpKFs7nuSHJpU-8G8nPfZAKbwt6phPTxpxqGz2892l26D78Qib4k5TvOKKzjJPr3DD1vKSh3sbjPbc/s1600/IMG_0041.JPG" imageanchor="1" style="clear: left; cssfloat: left; margin-bottom: 1em; margin-left: auto; margin-right: auto;"><img border="0" height="240" qea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiJeTXvB4UKUguL6f3ZjU8_JdJeh04cPOfYfWEZhjLg4G6PNeRxVuqWn_3RpeACWXpKFs7nuSHJpU-8G8nPfZAKbwt6phPTxpxqGz2892l26D78Qib4k5TvOKKzjJPr3DD1vKSh3sbjPbc/s320/IMG_0041.JPG" width="320" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;">Flysch claystone and sandstone skeletic bedrock</td></tr>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg5PdJDAwscAgZeGLJY-Sl1S3j1RsMKV_O4CSYO_hyfOFTXDfZ5XL-dFN-01QhfJQOhbWg88TcNbb04K_oH-GazTt7g0nAtV0AU5WPH5mV8xCwdcwFFJvAwNgILhebK0-189QPu1yJxkvs/s1600/IMG_0061.JPG" imageanchor="1" style="clear: left; cssfloat: left; margin-bottom: 1em; margin-left: auto; margin-right: auto;"><img border="0" height="150" qea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg5PdJDAwscAgZeGLJY-Sl1S3j1RsMKV_O4CSYO_hyfOFTXDfZ5XL-dFN-01QhfJQOhbWg88TcNbb04K_oH-GazTt7g0nAtV0AU5WPH5mV8xCwdcwFFJvAwNgILhebK0-189QPu1yJxkvs/s200/IMG_0061.JPG" width="200" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;">Beech primeval forest in the developmental stage of maturation</td></tr>
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Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-72205530159970198302012-10-31T14:07:00.002+01:002012-10-31T16:54:57.697+01:00Ranker modálny, Sitno<br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh_ORly-UMYFsxn9nyh0D1ZaOht-554CTpqTJCIYjWT1D4hrXPeSip7zDDCwbUctReXhMTCZs1zU1kvAu4GLr_Zh1AvSdjwxHSAbHu-2Usa2ORq-x0meZrMINtc-iUHIYfmP3Q7KFITLDA/s1600/IMG_0106.JPG" imageanchor="1" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img border="0" height="150" qea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh_ORly-UMYFsxn9nyh0D1ZaOht-554CTpqTJCIYjWT1D4hrXPeSip7zDDCwbUctReXhMTCZs1zU1kvAu4GLr_Zh1AvSdjwxHSAbHu-2Usa2ORq-x0meZrMINtc-iUHIYfmP3Q7KFITLDA/s200/IMG_0106.JPG" width="200" /></a></div>
<span style="font-family: "Trebuchet MS", sans-serif;">Location: Štiavnické vrchy Mts., Slovakia</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Elevation: 990 m a. s. l.</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Author of the photographies: P. Pišút ©, 11.10.2012</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Land use: Nature Reserve</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Vegetation: mixed Carpathian forest </span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification MKSP (2000): <a href="http://pedogeografiauk.blogspot.sk/2008/02/ranker-modlny-rmm.html">Ranker modálny</a></span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification WRB (2006): Skeletic Leptosol</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Parent rock: Andesite boulders </span><br />
<br />Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-44525110241596428932012-10-31T12:44:00.004+01:002012-10-31T12:48:55.292+01:00Luvizem kultizemná<span style="font-family: "Trebuchet MS", sans-serif;"><a href="http://pedogeografiauk.blogspot.sk/search?q=luvizem">Luvizem</a> s kultizemným ornicovým Akp-horizontom do hĺbky 35 cm.</span><br />
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<span style="font-family: Trebuchet MS;"><a href="http://pedogeografiauk.blogspot.sk/2012/07/luvizem-kultizemna-albic-luvisol.html">Luvizem kultizemná (1), Košariská</a></span>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-7668072962010641612012-10-30T17:55:00.006+01:002012-10-30T17:59:28.541+01:00Kambizem rendzinová (KMv) <span style="font-family: "Trebuchet MS", sans-serif;"><a href="http://pedogeografiauk.blogspot.sk/2008/01/kambizem.html">Kambizem</a> s alteračnými znakmi v Bv horizonte, podmienenými prevažne vylúhovaním karbonátov v časti pedonu pod A-horizontom a s karbonátovým C-horizontom.</span><br />
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<span style="font-family: Trebuchet MS;"><a href="http://pedogeografiauk.blogspot.sk/2012/10/kambizem-modalna-turecka.html">Kambizem rendzinová (1), Turecká</a> </span>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-61692309560920811142012-10-16T17:26:00.002+02:002012-10-31T12:51:00.151+01:00Kambizem rendzinová, Turecká<div class="separator" style="border-bottom: medium none; border-left: medium none; border-right: medium none; border-top: medium none; clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgPrKNO2OV7-C6p9zWs6SfxKLoJPwSKtJNP3qsHDzFFRQzQ44qjY3SlQCnWPKIY9TT3RriFQ_VtfAl4PHjlhcZLWS2nW_WI0fwSJN8hccd9e0pT5xG6_zrCkprssKBVO4vUcdTdyOfteP4/s1600/IMG_0071.JPG" imageanchor="1" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img border="0" height="150" nea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgPrKNO2OV7-C6p9zWs6SfxKLoJPwSKtJNP3qsHDzFFRQzQ44qjY3SlQCnWPKIY9TT3RriFQ_VtfAl4PHjlhcZLWS2nW_WI0fwSJN8hccd9e0pT5xG6_zrCkprssKBVO4vUcdTdyOfteP4/s200/IMG_0071.JPG" width="200" /></a></div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg_k4-ORJunYNk-YuHQ4-ivf8escsIINJ7MPhRzztLVNTPqWr_yF96P8mYOnbwC-I4fukKFpsGrX0Oh4kL1ZxgXDBFC6d7gt_aUmiSq6f17DlWP1OYlQF28P_kLhI51XvTP2s7JASh7_nY/s1600/IMG_0074.JPG" imageanchor="1" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img border="0" height="150" nea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg_k4-ORJunYNk-YuHQ4-ivf8escsIINJ7MPhRzztLVNTPqWr_yF96P8mYOnbwC-I4fukKFpsGrX0Oh4kL1ZxgXDBFC6d7gt_aUmiSq6f17DlWP1OYlQF28P_kLhI51XvTP2s7JASh7_nY/s200/IMG_0074.JPG" width="200" /></a><span style="font-family: "Trebuchet MS", sans-serif; font-size: x-small;">Cambic horizon, macrostructure</span></div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhhKimOorrQtnWimKqyBON_CTZW1hDcMWoHVPInV3FnYYgKPr7BV10-FzorG8GqAr50wVKuV2wmUYyPS9jBqt3aAWynXlIwBMMv88ssfKORKoDNFqYS2k9cG5GGi35VKxKKBCy8C4GgPPc/s1600/IMG_0080.JPG" imageanchor="1" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img border="0" height="200" nea="true" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhhKimOorrQtnWimKqyBON_CTZW1hDcMWoHVPInV3FnYYgKPr7BV10-FzorG8GqAr50wVKuV2wmUYyPS9jBqt3aAWynXlIwBMMv88ssfKORKoDNFqYS2k9cG5GGi35VKxKKBCy8C4GgPPc/s200/IMG_0080.JPG" width="150" /></a></div>
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<span style="font-family: "Trebuchet MS", sans-serif;">Location: Veľká Fatra Mts., Slovakia</span><br />
<span style="font-family: Trebuchet MS;">Elevation: 765 m a. s. l.</span></div>
<div style="border-bottom: medium none; border-left: medium none; border-right: medium none; border-top: medium none; clear: both; text-align: left;">
<span style="font-family: "Trebuchet MS", sans-serif;">Author of the photographies: P. Pišút ©, 12.10.2012</span></div>
<div style="border-bottom: medium none; border-left: medium none; border-right: medium none; border-top: medium none;">
<span style="font-family: "Trebuchet MS", sans-serif;">Land use: National Park, protective zone </span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Vegetation: mixed mountain Carpathian forest (European beech, maple)</span></div>
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<span style="font-family: "Trebuchet MS", sans-serif;">Classification MKSP (2000): <a href="http://pedogeografiauk.blogspot.sk/2012/10/kambizem-rendzinova-kmv.html">Kambizem rendzinová</a></span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification WRB (2006): Cambisol, eutric</span></div>
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<span style="font-family: "Trebuchet MS", sans-serif;">Parent rock: Weathering material derived from argillaceous lime/limestone (Triassic age)</span></div>
Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-75336433218906728192012-08-01T17:08:00.000+02:002012-10-31T15:45:08.825+01:00Rendzina modálna, Súľovské skaly<div class="separator" style="border-bottom: medium none; border-left: medium none; border-right: medium none; border-top: medium none; clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEizIzmVNJLVKxItw6I6aakbisXLaZJgDdyaH99Kcjr59CrEyB-_pZIZvWh7GkuFOXFyO6xrGyYJ-nyHS_LVw-5xfOpZkkCHil5SqwrzmoHYSJFuT-aaGC4U0ppPOkCvjbNQ-Hb4c03DQB4/s1600/IMG_0048.JPG" imageanchor="1" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img border="0" eda="true" height="150" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEizIzmVNJLVKxItw6I6aakbisXLaZJgDdyaH99Kcjr59CrEyB-_pZIZvWh7GkuFOXFyO6xrGyYJ-nyHS_LVw-5xfOpZkkCHil5SqwrzmoHYSJFuT-aaGC4U0ppPOkCvjbNQ-Hb4c03DQB4/s200/IMG_0048.JPG" width="200" /></a></div>
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<span style="font-family: "Trebuchet MS", sans-serif;">Location: Súľovské vrchy Mts., Slovakia</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Author of the photographies: P. Pišút ©, 30.4.2012</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Land use: Nature reserve Súľovské skaly</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Vegetation: mixed forest (European beech, Scots pine)</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification MKSP (2000): <a href="http://pedogeografiauk.blogspot.sk/2008/04/regozem-v-typickom-vvoji-bez-alch.html">Rendzina modálna</a></span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification WRB (2006): Rendzic Leptosol</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Parent rock: Calcareous conglomerate (Paleogene age)</span><br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhHthB7Z-Wf50o4-qJKKPqzb2ETwKGsiq7viLxGQ7DNLglbw3Y0l0ybfKt-cw6WH8Gk7NqoRX0Xt-_NtaG0incxjqn3EGez6z90xNhKKZDgxa16htr5NQsZJgSMW4ulHOaCe6d2maKduIo/s1600/IMG_0043.JPG" imageanchor="1" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img border="0" eda="true" height="176" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhHthB7Z-Wf50o4-qJKKPqzb2ETwKGsiq7viLxGQ7DNLglbw3Y0l0ybfKt-cw6WH8Gk7NqoRX0Xt-_NtaG0incxjqn3EGez6z90xNhKKZDgxa16htr5NQsZJgSMW4ulHOaCe6d2maKduIo/s200/IMG_0043.JPG" width="200" /></a><br />
<table cellpadding="0" cellspacing="0" class="tr-caption-container" style="float: left; margin-right: 1em; text-align: left;"><tbody>
<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj-tLUkoPdzw98jvoxOXN5bsbPSljPEa3_meplT7Oz9vghVxBbU7CZIYiEAeqNv-btNduhFYgLGYXmzeVb-WOQPz5ImvTHfQP29IGcHr6naT9X2sKt_h1QdHEmzlbNwQGM9Rp0QbVyNzg4/s1600/IMG_0033.JPG" imageanchor="1" style="clear: left; cssfloat: left; margin-bottom: 1em; margin-left: auto; margin-right: auto;"><img border="0" eda="true" height="150" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj-tLUkoPdzw98jvoxOXN5bsbPSljPEa3_meplT7Oz9vghVxBbU7CZIYiEAeqNv-btNduhFYgLGYXmzeVb-WOQPz5ImvTHfQP29IGcHr6naT9X2sKt_h1QdHEmzlbNwQGM9Rp0QbVyNzg4/s200/IMG_0033.JPG" width="200" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-family: "Trebuchet MS", sans-serif; font-size: x-small;">Paleogene conglomerate</span></td></tr>
</tbody></table>
Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-1356889397843164452012-08-01T15:50:00.002+02:002012-10-31T16:35:47.726+01:00Rendzina litozemná, Kláštorská roklina, Slovenský raj <br />
<div style="text-align: left;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiqbZSlRnhbW4SghcfbMPg6C9ewNAPA1YuMh_eB29_wFwou0YBb1dRakEbkrMsjU_UWf95fXzu-ghcN7KzWQt2EqQ45Q7fMgTgwBPa_u8qXJY1Ck6DQOm9GEcdVMlAg7Rqr6GowHaUEIYI/s1600/IMG_0070.JPG" imageanchor="1" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img border="0" eda="true" height="240" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiqbZSlRnhbW4SghcfbMPg6C9ewNAPA1YuMh_eB29_wFwou0YBb1dRakEbkrMsjU_UWf95fXzu-ghcN7KzWQt2EqQ45Q7fMgTgwBPa_u8qXJY1Ck6DQOm9GEcdVMlAg7Rqr6GowHaUEIYI/s320/IMG_0070.JPG" width="320" /></a></div>
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<span style="font-family: "Trebuchet MS", sans-serif;">Location: Slovenský raj Mts., Kláštorská roklina Gorge<br />Author of the photography: P.Pišút ©, 13.7.2012<br />Land use: Nature reserve (National park)<br />Vegetation: mixed forest (silver fir, European beech, Scots pine, spruce)<br />Classification MKSP (2000): <a href="http://pedogeografiauk.blogspot.sk/2009/07/rendzina-litozemna-raq.html">Rendzina litozemná</a></span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification WRB (2006): Rendzic Leptosol<br />Parent material / rock: limestone</span>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-16429431794114582182012-07-31T14:37:00.000+02:002012-10-31T12:47:04.428+01:00Luvizem kultizemná (1), Košariská<div class="separator" style="clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhAHRb4eElMPPAilRCa_QRQqrTq7LvxoWXV872dJPfFlJWv_r0CaJl0D15ZM0HgGeFLCLqwuF99a8bSVlSHBDgmEsa0piwo8G96Z5eTf7WFz_6my1uCE4YbosTlvcKyuugqNKFedH-F8QA/s1600/IMG_0002.JPG" imageanchor="1" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img border="0" eda="true" height="200" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhAHRb4eElMPPAilRCa_QRQqrTq7LvxoWXV872dJPfFlJWv_r0CaJl0D15ZM0HgGeFLCLqwuF99a8bSVlSHBDgmEsa0piwo8G96Z5eTf7WFz_6my1uCE4YbosTlvcKyuugqNKFedH-F8QA/s200/IMG_0002.JPG" width="163" /></a></div>
<span style="font-family: "Trebuchet MS", sans-serif;">Location: Myjava hillands, Slovakia</span><br />
<span style="font-family: Trebuchet MS;">Site: Košariská</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Author of the photography: P.Pišút © 30.7.2012</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Land use: farming cropland </span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification MKSP (2000): <a href="http://pedogeografiauk.blogspot.sk/2012/10/luvizem-kultizemna.html">Luvizem kultizemná</a></span><br />
<span style="font-family: "Trebuchet MS", sans-serif;"><span style="font-family: "Trebuchet MS", sans-serif;">Classification</span> WRB (2006): Albic Luvisol </span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Remarks: albic horizon; argic horizon </span><br />
<table cellpadding="0" cellspacing="0" class="tr-caption-container" style="float: left; margin-right: 1em; text-align: left;"><tbody>
<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiBvuENMOg5nhi-6aa6vGRzYJtbrjpADPbDUnndEo_B-riQVOwTrSsB1ycHhT8U1M1ohuJsIzPdsGdSJSBuJN_q1vju9jlU03I-5Zqv4w5xqgJr9VqGSZjbxzfKVbufCOHAXoSaNg9RxTo/s1600/IMG_0006.JPG" imageanchor="1" style="clear: left; cssfloat: left; margin-bottom: 1em; margin-left: auto; margin-right: auto;"><img border="0" eda="true" height="134" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiBvuENMOg5nhi-6aa6vGRzYJtbrjpADPbDUnndEo_B-riQVOwTrSsB1ycHhT8U1M1ohuJsIzPdsGdSJSBuJN_q1vju9jlU03I-5Zqv4w5xqgJr9VqGSZjbxzfKVbufCOHAXoSaNg9RxTo/s200/IMG_0006.JPG" width="200" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="background-color: black; font-family: "Trebuchet MS", sans-serif; font-size: x-small;">Argic horizon, transition into the C subsoil</span></td></tr>
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<table cellpadding="0" cellspacing="0" class="tr-caption-container" style="float: left; margin-right: 1em; text-align: left;"><tbody>
<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjD8MSh5sL4wc9s4j3LYVDArTmMBUZQ4iAEbRBwrcqmpM974X8xx4bx3mhPrVIek6xN2m6TsXWl12R3TUD0VjzFpfvsaFlKJD_01WRh9yUNu836UqLVjMEeRmIb_rTn9hFALOKuKUJ9qfE/s1600/IMG_0007.JPG" imageanchor="1" style="clear: left; cssfloat: left; margin-bottom: 1em; margin-left: auto; margin-right: auto;"><img border="0" eda="true" height="150" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjD8MSh5sL4wc9s4j3LYVDArTmMBUZQ4iAEbRBwrcqmpM974X8xx4bx3mhPrVIek6xN2m6TsXWl12R3TUD0VjzFpfvsaFlKJD_01WRh9yUNu836UqLVjMEeRmIb_rTn9hFALOKuKUJ9qfE/s200/IMG_0007.JPG" width="200" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="background-color: black; font-family: "Trebuchet MS", sans-serif; font-size: x-small;">Argic horizon, macrostructure</span></td></tr>
</tbody></table>
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Unknownnoreply@blogger.com0tag:blogger.com,1999:blog-9206919399764701712.post-5324540324423643072011-11-10T17:17:00.025+01:002012-11-05T17:13:50.687+01:00Hnedozem kultizemná (Luvisol)<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg8Rv6uaEJELHiGiRLTFvnCiDzQNbS-R1mlYMjivnRGA54fu7wtipF5HLSNGD5-91gboYX_PKxPf9X73q6ncLcjcCHOX7oRvWL68tKdJSU75ID4rfk2yAaajB1eFXRMQj7DeQiI5SnDOIY/s1600/IMG_0026.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5673404507471025138" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg8Rv6uaEJELHiGiRLTFvnCiDzQNbS-R1mlYMjivnRGA54fu7wtipF5HLSNGD5-91gboYX_PKxPf9X73q6ncLcjcCHOX7oRvWL68tKdJSU75ID4rfk2yAaajB1eFXRMQj7DeQiI5SnDOIY/s320/IMG_0026.JPG" style="cursor: hand; float: left; height: 320px; margin: 0px 10px 10px 0px; width: 110px;" /></a> <span style="font-family: trebuchet ms;">Location: Bernolákovo, Slovakia, Danubian Lowlands</span><br />
<span style="font-family: trebuchet ms;">Author of the photography: Peter Pišút ©</span><span style="font-family: trebuchet ms;">Parent material: loess</span><br />
<span style="font-family: Trebuchet MS;">Land use: farming cropland (woodland until 19th century)</span><br />
<span style="font-family: trebuchet ms;">Classification WRB (2006): Luvisol (siltic)</span><br />
<span style="font-size: 85%;"><span style="font-family: Trebuchet MS;">Remarks: argic horizon; calcareous subsoil</span></span><br />
<span style="font-family: Trebuchet MS; font-size: 85%;"></span><br />
<span style="font-size: 85%;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi0Od7JGvzWQlItsySNEL4vKbPvGZYCZgnF-qCBc3ZJdEPNjSD3pVmZeo2zlQNkXYFDYCHTch0hyphenhyphenXyulw-_LUxNQJDh449GJZyGTS6z8jFXKSt2_hpPk7-PmVUR-6_hDRPxQfvDL3m1eIE/s1600/IMG_0028.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5673697282416951282" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi0Od7JGvzWQlItsySNEL4vKbPvGZYCZgnF-qCBc3ZJdEPNjSD3pVmZeo2zlQNkXYFDYCHTch0hyphenhyphenXyulw-_LUxNQJDh449GJZyGTS6z8jFXKSt2_hpPk7-PmVUR-6_hDRPxQfvDL3m1eIE/s320/IMG_0028.JPG" style="cursor: hand; height: 240px; width: 320px;" /></a></span><br />
<span style="font-family: trebuchet ms; font-size: 85%;">Argic horizon (Bt horizont)</span>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-56706458081314539732010-05-17T14:07:00.006+02:002012-11-05T16:55:59.828+01:00Čiernica černozemná (ČAb)<a href="http://pedogeografiauk.blogspot.com/2008/01/iernica.html">Čiernica</a> s oxidačnými znakmi <a href="http://pedogeografiauk.blogspot.com/2008/02/glejov-horizont-g.html">glejového G-horizontu</a> v prechodnom A/C horizonte; bez <a href="http://pedogeografiauk.blogspot.com/2008/07/glejov-redukn-horizont-gr.html">glejového redukčného Gr-horizontu</a> do 100 cm od povrchu.<br />
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<a href="http://pedogeografiauk.blogspot.com/2010/05/ciernica-cernozemna-nekyje.html">Čiernica černozemná (kultizemná) (1), Vrakúň</a>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-50371688231482999942010-05-17T13:49:00.008+02:002012-08-01T17:47:49.075+02:00Čiernica černozemná (1), Vrakúň<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgadKi7iTjfhyVZzzUKonUyziTTA6NfqSfySXKlpzGyF0wBeh0m72BDJTpeOQy-dihbkvVLDOO4GgrsKeO-i1DpbFZiiVlqf7qj6BZJH4EkUeC2tyUcGsWm56Y5v8MYsOf03MQqAjktWn0/s1600/IMG_1604.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5472205334976048354" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgadKi7iTjfhyVZzzUKonUyziTTA6NfqSfySXKlpzGyF0wBeh0m72BDJTpeOQy-dihbkvVLDOO4GgrsKeO-i1DpbFZiiVlqf7qj6BZJH4EkUeC2tyUcGsWm56Y5v8MYsOf03MQqAjktWn0/s200/IMG_1604.JPG" style="cursor: hand; height: 90px; width: 200px;" /></a><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Location: Danubian Lowlands, Žitný ostrov Island, Slovakia</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Author of the photography: J. Procházka ©, 11.5.2010</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Land use: farming cropland</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Field position: inner bank of the former Danube channel near the village Vrakúň</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification MKSP (2000): </span><a href="http://pedogeografiauk.blogspot.com/2010/05/ciernica-cernozemna-cab.html"><span style="font-family: "Trebuchet MS", sans-serif;">Čiernica černozemná</span></a><span style="font-family: "Trebuchet MS", sans-serif;"> (kultizemná) </span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification WRB (2006): Mollic Fluvisol, Calcaric</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Parent material / rock: Calcareous alluvial loamy sands</span><br />
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<span style="font-family: trebuchet ms; font-size: 85%;">Profil:</span><br />
<span style="font-family: trebuchet ms; font-size: 85%;">0-35 Akpc, tmavosivý, farba 10 YR 2/1, silne karbonátový, súdržný, hlinitopiesočnatý</span><br />
<span style="font-family: trebuchet ms; font-size: 85%;">35-62 cm A/C(Go)c, silne karbonátový, piesočnato-hlinitý, nezreteľné hrdzavé škvrny do 10 %</span><br />
<span style="font-family: trebuchet ms; font-size: 85%;">62-72 C(Go) svetlohnedosivý piesok, ojedinelé hrdzavé škvrny, nekarbonátový</span><br />
<span style="font-family: trebuchet ms; font-size: 85%;">72-102 cm CGo nekarbonátový piesok, farba 10 YR 4,5/4, ojedinelé valúny štrku do 2 cm</span><br />
<span style="font-family: trebuchet ms; font-size: 85%;">102-125 cm CGro svetlohnedý nekarbonátový piesok, sivá + hnedá farebnosť, nepatrné, difúzne, stredne kontrastné hrdzavé škvrny.</span>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-15102494431390205862010-05-17T12:14:00.044+02:002010-05-17T14:30:13.813+02:00Čiernica glejová (2), Nekyje<span style="font-family:'Trebuchet MS', sans-serif;font-size:x-small;"><span style="font-size:small;"><a href="http://pedogeografiauk.blogspot.com/2008/12/iernica-glejov-ag.html">Čiernica glejová</a> na dne bývalého ramena Dunaja pri obci Nekyje, nadmorská výška 114 m n. m. Vlhká kosená lúka s metlicou trsnatou (<em>Deschampsia caespitosa</em>), ostricami (<em>Carex</em> spp.), kostihojom (<em>Symphytum officinale</em>), pichliačom sivým (<em>Cirsium canum</em>) a i. Foto (C) J. Procházka, 28.4.2010.</span> </span><br /><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg-LTDWstu5yENfP-b-HNkFaN5VhoM7S5dL9ghADv6MNtjyTxLDSqPIwyCA6pEo5cstjgMsJm3qsJc5QJ0zD-6B_yk3lhSqWW1C1FvhejmY6tO9bOij7CXRGb1C5_pbKBgHtEB4YBdk7z4/s1600/IMG_1527.JPG"><img style="WIDTH: 150px; HEIGHT: 200px; CURSOR: hand" id="BLOGGER_PHOTO_ID_5472215062113428994" border="0" alt="" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg-LTDWstu5yENfP-b-HNkFaN5VhoM7S5dL9ghADv6MNtjyTxLDSqPIwyCA6pEo5cstjgMsJm3qsJc5QJ0zD-6B_yk3lhSqWW1C1FvhejmY6tO9bOij7CXRGb1C5_pbKBgHtEB4YBdk7z4/s200/IMG_1527.JPG" /></a><br /><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><br /><span style="font-size:85%;">Profil:</span></div></div></div><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><span style="font-size:85%;">0-1 cm Oom, staré stonky metlice, mach</span></div></div></div><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><span style="font-size:85%;">0-25 cm Amčc, farba 10 YR 2,5/1,5, hlinitopiesočnatá zemina, drobnohrudkovitá štruktúra, stredne karbonátový, zreteľný prechod do</span></div></div></div><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><a href="http://pedogeografiauk.blogspot.com/2008/01/humolitov-horizont-oh.html"><span style="font-family:trebuchet ms;font-size:85%;">Oh</span></a><span style="font-family:trebuchet ms;font-size:85%;"> 25-36 cm, tmavý, farba 10 YR 3/1, piesočnatohlinitý, slabo karbonátový, bohatý na subfosílne ulity mokradných slimákov, zreteľný prechod do </span></div></div></div><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><a href="http://pedogeografiauk.blogspot.com/2008/07/raelinov-mezick-otm-horizont.html"><span style="font-family:trebuchet ms;font-size:85%;">Otm</span></a><span style="font-family:trebuchet ms;font-size:85%;"> 36-49 cm, minerálny podiel ílovitohlinitý, zreteľný, zvlnený prechod do </span></div><div style="BORDER-BOTTOM: medium none; BORDER-LEFT: medium none; BORDER-TOP: medium none; BORDER-RIGHT: medium none"><span style="font-size:85%;">Gr, uniformne sivý, farba 10 YR 5/1, ílovitý až íl, nevýrazne karbonátový, asi 15 % zvyškov pletív šachorovitých rastlín (<em>Cyperaceae</em>). Hladina podzemnej vody v 49 cm.</span></div></div></div>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-71283692929865049122010-05-14T16:31:00.004+02:002010-05-17T12:52:27.783+02:00Černozem modálna (kultizemná), Nekyje<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiYKIPwqmX8ZQ8mgxECtS0oQLsaK-rH8odAXbewZBz2PidcoF7BYa6Kfg8lXy_8sCBaN3LvaINn9IPcTvddfc4dBAVvcXov5LSNR2Kr6509loosYQGgYYm_kt-NrDx1GxdyzeltdW5DOug/s1600/IMG_1661.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5471133539895775202" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiYKIPwqmX8ZQ8mgxECtS0oQLsaK-rH8odAXbewZBz2PidcoF7BYa6Kfg8lXy_8sCBaN3LvaINn9IPcTvddfc4dBAVvcXov5LSNR2Kr6509loosYQGgYYm_kt-NrDx1GxdyzeltdW5DOug/s200/IMG_1661.JPG" style="cursor: hand; height: 200px; width: 150px;" /></a><br />
<span style="font-size: 85%;"><a href="http://pedogeografiauk.blogspot.com/2008/02/ernozem-modlna.html">Černozem modálna</a> (kultizemná), karbonátová, silne skeletnatá, z terasových štrkopieskov. Nekyje, vyvýšená vrcholová časť bývalej štrkovej zákrutovej lavice vo vnútri paleomeandra Dunaja, n. výška 115 m n. m. Foto (C) J. Procházka, 11.5.2010.</span><br />
<div><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjnklGt-LYvtXwvzP1eWAqEfEMZ9VDQrB41Wjt2wQ_IDT1x5j3nVPJ5kp2OCS7wvLJI84LDYRKg5-ZVnJOzX0lAok5H_ijow9_GbE0ITgsc926SUTuwgRhmKHLWWkvd_2k80nT33Pxylwk/s1600/IMG_1659.JPG" style="clear: left; cssfloat: left; float: left; margin-bottom: 1em; margin-right: 1em;"><img alt="" border="0" height="214" id="BLOGGER_PHOTO_ID_5471133535289266242" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjnklGt-LYvtXwvzP1eWAqEfEMZ9VDQrB41Wjt2wQ_IDT1x5j3nVPJ5kp2OCS7wvLJI84LDYRKg5-ZVnJOzX0lAok5H_ijow9_GbE0ITgsc926SUTuwgRhmKHLWWkvd_2k80nT33Pxylwk/s320/IMG_1659.JPG" style="height: 134px; width: 200px;" width="320" /></a> </div><div><br />
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<span style="font-size: 85%;">Profil:</span></div><div><span style="font-size: 85%;"><a href="http://pedogeografiauk.blogspot.com/2008/02/molick-karbontov-amc-horizont.html">Amc</a> (Akpc), 0-35 cm, sivočierny, farba 10 YR 2,5/1, prechod rovný, ostrý do:</span></div><div><span style="font-size: 85%;">Cc, sivohnedý štrkopiesok , bez oxidačno-redukčných znakov, slabo karbonátový, priemer valúnov štrku okolo 0,5 cm (max. 2,5 cm, ojedinele aj 7 cm).</span><br />
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh3HgZ7_PjjZnmy2RYUqeXrb2bzJz7Ek6eTsWtuqs5NvOIWmMdwH8QnxFDKXcecbKk2BwNfaDaQZsyC3YS0nyZJTg5iclbTypec_L3DsB2s8QK2NbslQ18YkQLfiiot92yt2RGWvfxmNLI/s1600/IMG_1672.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5471133545557455186" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh3HgZ7_PjjZnmy2RYUqeXrb2bzJz7Ek6eTsWtuqs5NvOIWmMdwH8QnxFDKXcecbKk2BwNfaDaQZsyC3YS0nyZJTg5iclbTypec_L3DsB2s8QK2NbslQ18YkQLfiiot92yt2RGWvfxmNLI/s200/IMG_1672.JPG" style="cursor: hand; height: 150px; width: 200px;" /></a></div><div><span style="font-family: trebuchet ms; font-size: 85%;">Ostrý prechod ornicového humusového horizontu do substrátových štrkopieskov s nevýraznými znakmi pôvodnej fluviálnej stratifikácie.</span> <span style="font-size: 85%;">Foto (C) J. Procházka, 11.5.2010.</span> </div>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-62987826982390292332010-05-12T16:14:00.001+02:002010-05-17T12:50:14.500+02:00Kambizem luvizemná (1), Železná Studnička<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEipYo_So3M501nfkJXACbB22EHArqlMrcdA0Ren3ENtvfespTzQ3zN_Wl5J4nmwVSCQXEfFBFpZd9YGBBWx_Danzdq3nN_2KpSKF1FGSP066T89LOr56snzij2HUA8f31_5GwKiaHQZO3s/s1600/pedo0009_vymol.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5470387248553201922" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEipYo_So3M501nfkJXACbB22EHArqlMrcdA0Ren3ENtvfespTzQ3zN_Wl5J4nmwVSCQXEfFBFpZd9YGBBWx_Danzdq3nN_2KpSKF1FGSP066T89LOr56snzij2HUA8f31_5GwKiaHQZO3s/s200/pedo0009_vymol.JPG" style="cursor: hand; height: 200px; width: 133px;" /></a><br />
<span style="font-size: 85%;"><a href="http://pedogeografiauk.blogspot.com/2010/05/kambizem-luvizemna-kml.html">Kambizem luvizemná</a> na mocnom podsvahovom delúviu. Odkryv v dolnej časti bývalého výmoľa lesnej cesty. Železná Studnička. Foto (C) Miloš Rusnák, 12.5.2010.</span><br />
<span style="font-size: 85%;">Profil:</span><br />
<span style="font-size: 85%;">(Ool) mach</span><br />
<span style="font-size: 85%;">Aoq, 0-10 cm, farba 10 YR 3/2, nekarbonátový, kyprý, piesočnatý. Zreteľný, šikmý, zvlnený prechod do<br />
<a href="http://pedogeografiauk.blogspot.com/2008/09/kambick-horizont-bv.html">Bv</a>, 10-90 cm, hrdzavohnedý, farba 10 YR 4/6, hlinitopiesočnatá textúra, nekarbonátový, difúzny, šikmý prechod do<br />
<a href="http://pedogeografiauk.blogspot.com/2008/09/kambick-luvick-bvt-horizont.html">Bvt</a>, 90-140 cm, svetlohnedý, farba 4,5/5, piesočnato-hlinitý. Zreteľný, šikmý prechod do<br />
Cc, 140-210 cm; silne karbonátový hlinitý piesok s prímesou spraše, farba 2.5 Y 6/4, elementárna štruktúra.</span><br />
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgsg-hQf6M9REl1E1Pz0Me-BLljA_c1mO3i4gNTEvwQZRXwdYgCWl3Bq586CfeHct8Z8NmVQGggNmslpf80BEh903VYS7ZIUqE_fbnR-NWUUodSDO9erOzla7RV5FymEuwiooRiuQ1LmB4/s1600/Pedo0019_KMl.JPG"><img alt="" border="0" height="320" id="BLOGGER_PHOTO_ID_5470387163149681346" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgsg-hQf6M9REl1E1Pz0Me-BLljA_c1mO3i4gNTEvwQZRXwdYgCWl3Bq586CfeHct8Z8NmVQGggNmslpf80BEh903VYS7ZIUqE_fbnR-NWUUodSDO9erOzla7RV5FymEuwiooRiuQ1LmB4/s320/Pedo0019_KMl.JPG" style="height: 200px; width: 146px;" width="233" /></a>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-59410741465934364552010-05-12T16:04:00.000+02:002010-05-12T16:23:36.107+02:00Kambizem luvizemná (KMl)<a href="http://pedogeografiauk.blogspot.com/2008/01/kambizem.html">Kambizem</a> s kambickým luvickým Bvt-horizontom aspoň v časti B-horizontu.<br /><br /><strong><span style="font-family:trebuchet ms;font-size:130%;">Aoq</span></strong><br /><strong><span style="font-family:trebuchet ms;font-size:130%;"><a href="http://pedogeografiauk.blogspot.com/2008/09/kambick-luvick-bvt-horizont.html">Bvt</a></span></strong><br /><strong><span style="font-family:trebuchet ms;font-size:130%;">B/C</span></strong><br /><strong><span style="font-family:trebuchet ms;font-size:130%;">C</span></strong><br /><strong><span style="font-family:Trebuchet MS;font-size:130%;"></span></strong><br /><span style="font-family:Trebuchet MS;"><a href="http://pedogeografiauk.blogspot.com/2010/05/kambizem-luvizemna-1-zelezna-studnicka.html">Kambizem luvizemná (1), Železná Studnička</a></span>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-3509539807422080222009-12-14T16:30:00.001+01:002012-10-31T16:06:46.819+01:00Čiernica organozemná (1), Nekyje<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgnl7NjNi6yf2BbpWlFMJCGT47CFEZNiju-6jmwKuG4Wzqyjj1O6PQ7zogSB60Gj4xaUUClFjRNIKm9iLVnNBDR0OiUS6O3VY1PL4egPeuLKG8hYMAf3-RqAyiV5ZMGV1o5ux0nTvixw30/s1600-h/IMG_2377.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5415114852216499058" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgnl7NjNi6yf2BbpWlFMJCGT47CFEZNiju-6jmwKuG4Wzqyjj1O6PQ7zogSB60Gj4xaUUClFjRNIKm9iLVnNBDR0OiUS6O3VY1PL4egPeuLKG8hYMAf3-RqAyiV5ZMGV1o5ux0nTvixw30/s200/IMG_2377.JPG" style="cursor: hand; height: 150px; width: 200px;" /></a><br />
<span style="font-family: Trebuchet MS;"><a href="http://pedogeografiauk.blogspot.com/2009/12/ciernica-organozemna-cat.html"><span style="font-size: 85%;">Čiernica organozemná</span></a><span style="font-size: 85%;">, dno zaniknutého dunajského ramena pri obci Nekyje. Foto 16.9.2009</span></span><span style="font-size: 85%;"> (c) P.Pišút.</span> <span style="font-family: trebuchet ms; font-size: 85%;">Hladina podzemnej vody v čase vzorkovania v hĺbke 1 m.</span><br />
<span style="font-family: Trebuchet MS; font-size: 85%;">Profil:</span><br />
<span style="font-family: Trebuchet MS; font-size: 85%;">0-1 cm <a href="http://pedogeografiauk.blogspot.com/2008/07/subhorizont-opadu-ool.html">Ool</a> staré stonky trste (<em>Phragmites australis</em>)</span><br />
<span style="font-family: Trebuchet MS; font-size: 85%;">0-40 cm <a href="http://pedogeografiauk.blogspot.com/2008/02/molick-iernicov-horizont-am.html">Amč</a></span><br />
<span style="font-family: Trebuchet MS; font-size: 85%;">40-55 cm A/Oh</span><br />
<span style="font-family: Trebuchet MS; font-size: 85%;">55-80 cm <a href="http://pedogeografiauk.blogspot.com/2008/01/humolitov-horizont-oh.html">Oh</a></span><br />
<span style="font-family: Trebuchet MS; font-size: 85%;">80-120 cm <a href="http://pedogeografiauk.blogspot.com/2008/07/raelinov-folick-otl-horizont.html">Otl</a> slatinná rašelina.</span><br />
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhPhlqWT3C2WCze5mgH8EWpWpsy5jValNDuneKZLeNbyHUHTla0sKVtm1YPt2DNBxezuY-BALkr2RsiGnv3aXQI6eQ6X8Bxl4Dw9UmBRLvEbNCSLv5zHec9mBapU3t9-XmLgEKNnMJZ63M/s1600-h/IMG_2378.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5415114862653638226" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhPhlqWT3C2WCze5mgH8EWpWpsy5jValNDuneKZLeNbyHUHTla0sKVtm1YPt2DNBxezuY-BALkr2RsiGnv3aXQI6eQ6X8Bxl4Dw9UmBRLvEbNCSLv5zHec9mBapU3t9-XmLgEKNnMJZ63M/s200/IMG_2378.JPG" style="cursor: hand; height: 150px; width: 200px;" /></a><br />
<span style="font-family: trebuchet ms; font-size: 85%;">Molický čiernicový horizont <a href="http://pedogeografiauk.blogspot.com/2008/02/molick-iernicov-horizont-am.html">Amč</a>, polodetail.</span><br />
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj0lCElnnLikK8T2ASxjj9lPbHOfuR3N-7pUGUrAkmFfi_3JaY5p39B7rqVm3oZhoEAB7qJQms9Qy0Yjycotyhpv7ZHC5G-6qBpaYbvqzUZis-7FR_B5BG_rq_HKuVm8GT8vYiRMgvs9zw/s1600-h/IMG_2382.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5415114863508593650" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj0lCElnnLikK8T2ASxjj9lPbHOfuR3N-7pUGUrAkmFfi_3JaY5p39B7rqVm3oZhoEAB7qJQms9Qy0Yjycotyhpv7ZHC5G-6qBpaYbvqzUZis-7FR_B5BG_rq_HKuVm8GT8vYiRMgvs9zw/s200/IMG_2382.JPG" style="cursor: hand; height: 150px; width: 200px;" /></a><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgUpaqS9MF0e3kw89xTvHFM0LZGb5UPOxaPp41HTGr1MHj-96_57pDAmvN_BKUN1t73YUQh_m6tmJD7EPZzL3vij8i5OHfy_y2V4ZpuRhAl57frud_uJOM-AGdFIXM-1RA4wulwK6AYQQg/s1600-h/IMG_2383.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5415114863715349970" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgUpaqS9MF0e3kw89xTvHFM0LZGb5UPOxaPp41HTGr1MHj-96_57pDAmvN_BKUN1t73YUQh_m6tmJD7EPZzL3vij8i5OHfy_y2V4ZpuRhAl57frud_uJOM-AGdFIXM-1RA4wulwK6AYQQg/s200/IMG_2383.JPG" style="cursor: hand; height: 150px; width: 200px;" /></a><br />
<span style="font-family: trebuchet ms; font-size: 85%;">Vegetácia: Ruderalizovaný porast trste (<em>Phragmites asutralis</em>) s pŕhľavou (<em>Urtica dioica</em>), povojou (<em>Calystegia sepium</em>), tiež lipkavec (<em>Galium aparine</em>), ostružina ožinová (<em>Rubus caesius</em>), zlatobyľ obrovská (<em>Solidago gigantea</em>), tiež stará suchá baza (<em>Sambucus nigra</em>).</span>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-90661974918618522332009-12-14T16:20:00.000+01:002009-12-15T17:29:07.731+01:00Čiernica organozemná (ČAt)<span style="font-family:trebuchet ms;"><a href="http://pedogeografiauk.blogspot.com/2008/01/iernica.html">Čiernica</a> s náznakmi rašelinového Ot-horizontu (hrúbky za vlhka do 30 cm), alebo s humolitovým <a href="http://pedogeografiauk.blogspot.com/2008/01/humolitov-horizont-oh.html">Oh-horizontom</a> hrúbky do 50 cm, s prechodom do molického čiernicového <a href="http://pedogeografiauk.blogspot.com/2008/02/molick-iernicov-horizont-am.html">Amč-horizontu</a>.</span><br /><span style="font-family:trebuchet ms;"></span><br /><span style="font-family:trebuchet ms;font-size:130%;"><a href="http://pedogeografiauk.blogspot.com/2008/02/molick-iernicov-horizont-am.html">Amč</a>-(Ot)-CG</span><br /><span style="font-family:trebuchet ms;font-size:130%;"><a href="http://pedogeografiauk.blogspot.com/2008/02/molick-iernicov-horizont-am.html">Amč</a>-<a href="http://pedogeografiauk.blogspot.com/2008/01/humolitov-horizont-oh.html">Oh</a>-Ot</span><br /><br /><span style="font-family:trebuchet ms;"><a href="http://pedogeografiauk.blogspot.com/2009/12/ciernica-organozemna-1-nekyje.html">Čiernica organozemná (1), Nekyje</a></span>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-55109948767467838222009-12-14T16:04:00.001+01:002009-12-14T16:20:17.854+01:00Čiernica kultizemná (3), Nekyje<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhrzB3DsCRQtVeYKQvxP4gA2_Tne96TG7R4M8hZzBeObFX5J0fhKQGSvKZ9b8oCUFSoyoxcT-4nsqCJ7kITJefS5vTdtX9BBbnfW4hMJaPN9O_z6_qMNSkbICgXcAKFxFyO1WCBR3Blons/s1600-h/IMG_2409.JPG"><img style="WIDTH: 150px; HEIGHT: 200px; CURSOR: hand" id="BLOGGER_PHOTO_ID_5415108963179715714" border="0" alt="" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhrzB3DsCRQtVeYKQvxP4gA2_Tne96TG7R4M8hZzBeObFX5J0fhKQGSvKZ9b8oCUFSoyoxcT-4nsqCJ7kITJefS5vTdtX9BBbnfW4hMJaPN9O_z6_qMNSkbICgXcAKFxFyO1WCBR3Blons/s200/IMG_2409.JPG" /></a><br /><div><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg8SaZgOJM_ELUkh9V62Q1WXrCxbsa_nQD30QhM8fNvSCWGPyytPOYuzEvbnMGM9TjEdAaYC1QHQsSoQSJ7gbugL9cQ93SPgVYcS0uj4uoRQqrauAyr38_YzvT6IhyphenhyphenCKgtS9-NvpMAApnk/s1600-h/IMG_2419.JPG"><img style="WIDTH: 200px; HEIGHT: 150px; CURSOR: hand" id="BLOGGER_PHOTO_ID_5415111829935672434" border="0" alt="" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg8SaZgOJM_ELUkh9V62Q1WXrCxbsa_nQD30QhM8fNvSCWGPyytPOYuzEvbnMGM9TjEdAaYC1QHQsSoQSJ7gbugL9cQ93SPgVYcS0uj4uoRQqrauAyr38_YzvT6IhyphenhyphenCKgtS9-NvpMAApnk/s200/IMG_2419.JPG" /></a></div>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-36851636444472012872009-12-11T14:56:00.003+01:002010-05-14T17:05:25.145+02:00Čiernica modálna (ČAm)<span style="font-family: trebuchet ms;"><a href="http://pedogeografiauk.blogspot.com/2008/01/iernica.html">Čiernica</a> s oxidačnými znakmi (škvrny, zhluky a noduly Fe alebo Mn) v <a href="http://pedogeografiauk.blogspot.com/2008/02/molick-iernicov-horizont-am.html">molickom čiernicovom Amč-horizonte</a>; bez glejového redukčného Gr-horizontu v hĺbke do 100 cm. </span><br />
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<strong><span style="font-family: trebuchet ms; font-size: 130%;"><a href="http://pedogeografiauk.blogspot.com/2008/02/molick-iernicov-horizont-am.html">Amč</a></span></strong><br />
<strong><span style="font-family: trebuchet ms; font-size: 130%;">A/CGo</span></strong><br />
<strong><span style="font-family: trebuchet ms; font-size: 130%;">CGo</span></strong><br />
<strong><span style="font-family: trebuchet ms; font-size: 130%;"><a href="http://pedogeografiauk.blogspot.com/2008/07/glejov-redukno-oxidan-horizont-gro.html">Gro</a></span></strong><br />
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<span style="font-family: trebuchet ms;"><a href="http://pedogeografiauk.blogspot.com/2009/12/ciernica-modalna-jurova.html">Čiernica modálna (1), Jurová</a></span>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-64594058618825508802009-12-04T12:12:00.000+01:002012-10-31T12:35:32.546+01:00Čiernica modálna, Jurová<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjUEsf0-bf-5T43SltTRBpxvyIBgV_AdQ_NbnPGOhxMjYp2_NN_MEB6ucn1peDDh3nQlgLTN2zCjNEiA7-ZXKv1xjR0cLJYtIUqo20F2en46rVmgNhW3bvivP3SvZQ83AtSZHSpmfFxnlE/s1600-h/CA.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5411337782636894738" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjUEsf0-bf-5T43SltTRBpxvyIBgV_AdQ_NbnPGOhxMjYp2_NN_MEB6ucn1peDDh3nQlgLTN2zCjNEiA7-ZXKv1xjR0cLJYtIUqo20F2en46rVmgNhW3bvivP3SvZQ83AtSZHSpmfFxnlE/s200/CA.JPG" style="cursor: hand; height: 200px; width: 143px;" /></a> <a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgXxwlOH4yDeI64BL0VYhsQufw5BpbONmIBhh3syzhV03-LgOL2bR-cWkjxvGUMl4rMP-cjQBCmTF-RgQMRFh77ucWuczjHJS-nS0LYLKinMei3bBiwQMqr_vGaREGANZlcdNyO82GhtkE/s1600-h/3_Cg.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5411337595391331042" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgXxwlOH4yDeI64BL0VYhsQufw5BpbONmIBhh3syzhV03-LgOL2bR-cWkjxvGUMl4rMP-cjQBCmTF-RgQMRFh77ucWuczjHJS-nS0LYLKinMei3bBiwQMqr_vGaREGANZlcdNyO82GhtkE/s200/3_Cg.JPG" style="cursor: hand; height: 200px; width: 150px;" /></a><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Location: Žitný ostrov Island, Slovakia</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Site: Jurová</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Elevation: 116 m a. s. l.</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Author of the photographies: S. Vércseová and M. Koli ©, 27.11.2009</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Land use: isolated forest</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Vegetation: forest edge of Poplar monoculture</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification MKSP (2000): </span><a href="http://pedogeografiauk.blogspot.com/2009/12/ciernica-modalna-cam.html"><span style="font-family: "Trebuchet MS", sans-serif;">Čiernica modálna</span></a><span style="font-family: "Trebuchet MS", sans-serif;">, karbonátová. </span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Classification WRB (2006): Mollic Fluvisol, with fossil organic horisons</span><br />
<span style="font-family: "Trebuchet MS", sans-serif;">Parent rock: alluvial loamy sand </span><br />
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<span style="font-size: 85%;">Profil: </span><br />
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<span style="font-size: 85%;">0-5 Om</span></div>
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<span style="font-size: 85%;">0-40 Am1c, drobnohrudkovitá štruktúra, piesočnato-hlinitá zemina, pravdepodobne antropicky ovplyvnený (celoplošnou úpravou pôdy pri zakladaní porastu); pH (vo vode) 8.22</span></div>
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<span style="font-size: 85%;">40-60 Am2c, hnedočierny, hlinitopiesočnatý, pH 8.28</span></div>
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<span style="font-size: 85%;">60-70 A/Cc </span></div>
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<span style="font-size: 85%;">70-125 CGroc, piesok, dominantné, stredne kontrastné hrdzavé škvrny nad 50 %, pH 8.08</span></div>
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<span style="font-size: 85%;">pod 125 Oh fosílny humolit, tmavý, ílovitá textúra, silne plastický, škvrny do 20 %, pH 7.94. </span></div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjrNGugoWkEO-Q8d0NgrYEn6rEbPjq2li5kRvc6tjkw6ad_lvqgddMn8SX7pLfxJp3Id0aJjQC-njD0-Enso9uMDrraJBKZwqV7XT242c3VhlbmrwGctLpbSWSg1gmYTlWrH9xHbZWgTno/s1600-h/SV.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5411337846057252786" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjrNGugoWkEO-Q8d0NgrYEn6rEbPjq2li5kRvc6tjkw6ad_lvqgddMn8SX7pLfxJp3Id0aJjQC-njD0-Enso9uMDrraJBKZwqV7XT242c3VhlbmrwGctLpbSWSg1gmYTlWrH9xHbZWgTno/s200/SV.JPG" style="cursor: hand; height: 150px; width: 200px;" /></a> <br />
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Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-20843476767939913542009-08-07T16:57:00.001+02:002012-10-31T16:06:13.105+01:00Organozem slatinná (2), Nekyje<span style="font-size: 85%;"><span style="font-family: Trebuchet MS;"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5367245179173072786" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgBC5JQvHwCJvLV6WKnQnj7F544pqWwswZLlrBfQ6NniC3IHEGkFOhKb64c2wP5uWQ3YplGHG_WegRtkycvuCWEQKwpt3IOSycN-WR4eXoW_Px0okkK_mXgpDwNrhox2wegWIgetVe-C7o/s200/IMG_1104.JPG" style="cursor: hand; float: left; height: 150px; margin: 0px 10px 10px 0px; width: 200px;" />O<a href="http://pedogeografiauk.blogspot.com/2008/07/organozem-glejov-omg.html">rganozem slatinná</a> na dne paleomeandra Dunaja pri obci Nekyje, Podunajská rovina, Žitný ostrov.</span> Foto 6.8.2009 © P.Pišút.</span><br />
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh7Mhkrq5BM-hl3ovApTbOG84EEvWJ9WkZx3H7Juh5wGEGlHvv_P-bWxgYUX94t6iDXNxzOSidiiFa4r2o1Zo0zyD_oLROICu4OFaR6P3wGCcRBcjsjH7Amav38hnhVjqPfelbTuWDw6Vw/s1600-h/IMG_1102.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5367242788755743442" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh7Mhkrq5BM-hl3ovApTbOG84EEvWJ9WkZx3H7Juh5wGEGlHvv_P-bWxgYUX94t6iDXNxzOSidiiFa4r2o1Zo0zyD_oLROICu4OFaR6P3wGCcRBcjsjH7Amav38hnhVjqPfelbTuWDw6Vw/s200/IMG_1102.JPG" style="cursor: hand; height: 150px; width: 200px;" /></a><br />
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<span style="font-size: 85%;">Profil:</span></div>
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<span style="font-size: 85%;">0-1 cm <a href="http://pedogeografiauk.blogspot.com/2008/09/mainov-hydromorfn-horizont-omh.html">Omh</a></span></div>
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<span style="font-size: 85%;">0-22 cm <a href="http://pedogeografiauk.blogspot.com/2008/01/humolitov-horizont-oh.html">Oh</a> (s ojedinelými subfosílnymi schránkami močiarnych mäkkýšov)</span></div>
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<span style="font-size: 85%;">22-100 cm <a href="http://pedogeografiauk.blogspot.com/2008/07/raelinov-folick-otl-horizont.html">Otl</a>, slatinná rašelina zo zvyškov trste a šachorovitých rastlín (<em>Cyperaceae</em>), výrazný zápach (redukčné prostredie). Hladina podzemnej vody v hĺbke 15 cm. <a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgTiWiO1ORpBBNcij4eXG4pdwh15gYOt_r9Mmsng7Caw_MZ_Lzghs7QjLBixcAsimzA3cuwjnU0d3fvRaXFH3nyORqtO0UbvZ4fkyaeIOCaKoHD096t_xDxhA6EBtc1jGsdTaQpwxUvnWM/s1600-h/IMG_1092.JPG"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5367240517476796994" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgTiWiO1ORpBBNcij4eXG4pdwh15gYOt_r9Mmsng7Caw_MZ_Lzghs7QjLBixcAsimzA3cuwjnU0d3fvRaXFH3nyORqtO0UbvZ4fkyaeIOCaKoHD096t_xDxhA6EBtc1jGsdTaQpwxUvnWM/s200/IMG_1092.JPG" style="cursor: hand; float: left; height: 150px; margin: 0px 10px 10px 0px; width: 200px;" /></a></span></div>
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<span style="font-family: trebuchet ms; font-size: 85%;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgpLDffiZJjThPQH26xN4Z65swBsZyZ6p9hteB8gBlzkfVtD5ERKtcGJB3P0rmcOaiQyi99jRNdtk1BwWxsKCqOdX5NSKvyhFK8RFuN4kggPF4_bklvqleHkh2mp-aCJVuisj-J_VtKKDs/s1600-h/IMG_1092.JPG"><span style="font-family: trebuchet ms; font-size: 85%;"></span></a><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh34k8c5HNyS0c4lmUcMa7_eu8i7JwjFVGPbWPn6hZSpAT-y-RwaHKi6Db0SPqJDs-D9sMfyrNCZ0rht5QL6VSwdquEU0IE3DSu-hX5p1w7EGy0gKeflvIPqFlo_k7U7-zS1YU-mSh-caw/s1600-h/IMG_1096.JPG"><span style="font-family: trebuchet ms; font-size: 85%;"><img alt="" border="0" id="BLOGGER_PHOTO_ID_5367236447391951282" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh34k8c5HNyS0c4lmUcMa7_eu8i7JwjFVGPbWPn6hZSpAT-y-RwaHKi6Db0SPqJDs-D9sMfyrNCZ0rht5QL6VSwdquEU0IE3DSu-hX5p1w7EGy0gKeflvIPqFlo_k7U7-zS1YU-mSh-caw/s200/IMG_1096.JPG" style="cursor: hand; float: left; height: 150px; margin: 0px 10px 10px 0px; width: 200px;" /></span></a></span></div>
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Stanovište: Kosený bylinno-travinný porast s dominanciou ostrice (Carex sp.) a ďalšími močiarnymi a vlhkomilnými rastlinami (<em>Mentha aquatica, Lythrum salicaria, Ranunculus repens</em>) na trvalo podmáčanom stanovišti s vysoko položenou hladinou podzemnej vody aj po odvodnení. Foto © P.Pišút.<br /><div>
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Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-27825551268073681092009-07-28T17:27:00.000+02:002012-08-01T16:07:59.489+02:00Rendzina litozemná (RAq)<span style="font-family: trebuchet ms;"><a href="http://pedogeografiauk.blogspot.com/2008/01/rendzina.html">Rendzina</a> s nástupom súvislej pevnej karbonátovej horniny v hĺbke 10-30 cm od povrchu.</span><br />
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<a href="http://pedogeografiauk.blogspot.com/2008/02/molick-karbontov-amc-horizont.html"><span style="font-family: trebuchet ms; font-size: 130%;"><strong>Amc</strong></span></a><span style="font-family: trebuchet ms; font-size: 130%;"><strong>-Rc</strong></span><br />
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<a href="http://pedogeografiauk.blogspot.com/2009/07/rendzina-litozemna-1-velky-choc.html">Rendzina litozemná (1), Veľký Choč</a><br />
<a href="http://pedogeografiauk.blogspot.sk/2012/08/rendzina-litozemna-klastorska-roklina.html">Rednzina litozemná, Kláštorská roklina, Slovenský raj</a>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-59373131722452726212009-07-28T17:02:00.000+02:002009-08-14T11:33:58.752+02:00Rendzina litozemná (1), Veľký Choč<span style="font-family:Trebuchet MS;font-size:85%;"><a href="http://pedogeografiauk.blogspot.com/2009/07/rendzina-litozemna-raq.html">Rendzina litozemná</a>. vylúhovaná, Chočské vrchy, JZ svah pod hrebeňom Veľkého Choča, n. výška 1 400 m n. m. </span><span style="font-family:Trebuchet MS;font-size:85%;">Foto 21.7.2009 © P.Pišút. <a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiteokO_4rB2JPQgs-EXTIUrGyzqf8HSkZf1qCDtiIiXXNeyr3WKFYXf5N9leQkUnIFnC_96FWMylEpfPqPXDAkj83TGUVAYSQdkJJJyNw-P5lqOKmxjB05Oua8CZq9vnTTxFFBDlE_Wzo/s1600-h/IMG_0834.JPG"><img style="MARGIN: 0px 10px 10px 0px; WIDTH: 200px; FLOAT: left; HEIGHT: 150px; CURSOR: hand" id="BLOGGER_PHOTO_ID_5363531192838271042" border="0" alt="" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiteokO_4rB2JPQgs-EXTIUrGyzqf8HSkZf1qCDtiIiXXNeyr3WKFYXf5N9leQkUnIFnC_96FWMylEpfPqPXDAkj83TGUVAYSQdkJJJyNw-P5lqOKmxjB05Oua8CZq9vnTTxFFBDlE_Wzo/s200/IMG_0834.JPG" /></a></span> <span style="font-family:trebuchet ms;font-size:85%;">Profil:</span><br /><span style="font-family:trebuchet ms;font-size:85%;">0-2 Om</span><br /><span style="font-family:trebuchet ms;font-size:85%;">0-7 cm Am, 10 % skeletu, drobnohrudkovitá štruktúra, bez karbonátov</span><br /><span style="font-family:trebuchet ms;font-size:85%;">7-25 cm A/Cc, vápencový skelet 40-50 %, priemerná veľkosť klastov 2-3 cm, max. 10 cm,</span><br /><span style="font-family:trebuchet ms;font-size:85%;">25 Rc.</span><br /><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjpfOzE3RG3Mf6iq3Ibji7PbAftxm7hyX-HGChbBJSaxhieNPxcmTqvDYuQgfaQmy0d3cAwZaygMAFLa31u2xLSFSvVJteb1hp90ErwjQc10_OGKfOKqZ51qApeBGCvskusE7MIPTFGCgU/s1600-h/IMG_0837.JPG"><img style="WIDTH: 200px; HEIGHT: 150px; CURSOR: hand" id="BLOGGER_PHOTO_ID_5363527290437582466" border="0" alt="" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjpfOzE3RG3Mf6iq3Ibji7PbAftxm7hyX-HGChbBJSaxhieNPxcmTqvDYuQgfaQmy0d3cAwZaygMAFLa31u2xLSFSvVJteb1hp90ErwjQc10_OGKfOKqZ51qApeBGCvskusE7MIPTFGCgU/s200/IMG_0837.JPG" /></a><br /><span style="font-family:trebuchet ms;font-size:85%;">Molický horizont, polodetail.</span><br /><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgcRiY1sr2EqZX-ni3ETd2UdfI2_X3Hp6RGtv1Pc7VaNya3yZwtCG_VtRipXAVctIeSSydLYNy-O1SCF4QBvopw00mNGIgGw1TFLobm_GkH9tYXO4dbhEmTjm0bANjRN_kb1JBNpmMiWT8/s1600-h/IMG_0840.JPG"><img style="WIDTH: 200px; HEIGHT: 150px; CURSOR: hand" id="BLOGGER_PHOTO_ID_5363527303590043842" border="0" alt="" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgcRiY1sr2EqZX-ni3ETd2UdfI2_X3Hp6RGtv1Pc7VaNya3yZwtCG_VtRipXAVctIeSSydLYNy-O1SCF4QBvopw00mNGIgGw1TFLobm_GkH9tYXO4dbhEmTjm0bANjRN_kb1JBNpmMiWT8/s200/IMG_0840.JPG" /></a><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhUGbZfdtdFWs11zHANrrN-mmiHxZ2vHpU7Ihqy6E-vvnN_klgG_ZxI_wqrNFcDw2V4YrOgyoaRUc-8iushAU9Eqb4HrN70ZoOM0J4plJWHqrE4kJXz8R8SOdJ5NjnU3n2LpfbG3amWaSM/s1600-h/IMG_0833.JPG"><img style="WIDTH: 200px; HEIGHT: 150px; CURSOR: hand" id="BLOGGER_PHOTO_ID_5363527310286227026" border="0" alt="" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhUGbZfdtdFWs11zHANrrN-mmiHxZ2vHpU7Ihqy6E-vvnN_klgG_ZxI_wqrNFcDw2V4YrOgyoaRUc-8iushAU9Eqb4HrN70ZoOM0J4plJWHqrE4kJXz8R8SOdJ5NjnU3n2LpfbG3amWaSM/s200/IMG_0833.JPG" /></a><br /><span style="font-family:trebuchet ms;font-size:85%;">Erózia pôdy pri turistickom chodníku.</span>Unknownnoreply@blogger.comtag:blogger.com,1999:blog-9206919399764701712.post-34725803399492469062009-07-28T14:52:00.000+02:002009-07-28T14:55:26.776+02:00Antrozemný iniciálny Adi horizont<span style="font-family:trebuchet ms;">Primitívne štádium tvorby pôd z antropogénnych materiálov, pričom hrúbka úložného materiálu je nad 35 cm. Súčasť <a href="http://pedogeografiauk.blogspot.com/2009/07/antrozem-inicialna-ana.html">iniciálnych antrozemí</a>.</span>Unknownnoreply@blogger.com