Methods for quantitative diagnostics of degree of hydromorphism of chernozem-like soils (based on example of soils of northern Tambov Plain)
The hydrologic features of chernozem-like soils of the northern Tambov Plain reflect the crystallinity of nonsilicate iron contained in ferromagnetic concretions, as well as the qualitative humus content and other properties. The possibility of using Schwertmann’s criterion and swampiness coefficien...
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| Veröffentlicht in: | Moscow University soil science bulletin 2012-03, Vol.67 (1), p.8-13 |
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| container_title | Moscow University soil science bulletin |
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| creator | Zaidelman, F. R. Nikiforova, A. S. Stepantsova, L. V. Krasin, V. N. |
| description | The hydrologic features of chernozem-like soils of the northern Tambov Plain reflect the crystallinity of nonsilicate iron contained in ferromagnetic concretions, as well as the qualitative humus content and other properties. The possibility of using Schwertmann’s criterion and swampiness coefficient in the Zaidel’man-Ogleznev method as diagnostic indices of degree of hydromorphism is shown. A new diagnostic index is suggested, i.e., the hydromorphism criterion (K
I–II
); the relation of the optical density of the extraction of alkaline and alkaline pyrophosphate from fine-earth arable land horizon is based on its definition. |
| doi_str_mv | 10.3103/S0147687412010097 |
| format | Article |
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I–II
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I–II
); the relation of the optical density of the extraction of alkaline and alkaline pyrophosphate from fine-earth arable land horizon is based on its definition.</description><subject>Diagnostics</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Historical Geology</subject><subject>Paleontology</subject><subject>Soils</subject><issn>0147-6874</issn><issn>1934-7928</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNp1kM1OwzAQhC0EEqXwANwsTnAI2I4TJ0dU8ScVgUQ5R3a8aVySOLXTivIMPDQJQeKAOO1oZ75daRA6peQypCS8eiGUizgRnDJCCUnFHprQNOSBSFmyjyaDHQz-ITryfkVIFDNOJujzEbrSao8L6_B6I5vOdLIzW8DayGVjfWdyj22BNSwdwKDKnXa2tq4tja-HRV6Ca-wH1EFl3gB7ayqPz5X0oLFtMLzLuq2-0dHqRWNdN1B4IWtlt_i5kqa5OEYHhaw8nPzMKXq9vVnM7oP5093D7Hoe5JQyERQ8oqHUKuKR5kJEhMU8kRFTmhRK0EhwwRhwCSGLFCgeK0WJEExrDSRhIpyis_Fu6-x6A77LVnbjmv5llvZ1xWESpn2IjqHcWe8dFFnrTC3dLqMkGzrP_nTeM2xkfJ9tluB-D_8PfQEv9ISw</recordid><startdate>20120301</startdate><enddate>20120301</enddate><creator>Zaidelman, F. R.</creator><creator>Nikiforova, A. S.</creator><creator>Stepantsova, L. V.</creator><creator>Krasin, V. N.</creator><general>Allerton Press, Inc</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope></search><sort><creationdate>20120301</creationdate><title>Methods for quantitative diagnostics of degree of hydromorphism of chernozem-like soils (based on example of soils of northern Tambov Plain)</title><author>Zaidelman, F. R. ; Nikiforova, A. S. ; Stepantsova, L. V. ; Krasin, V. N.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c1127-f4513adb545d477502648a52bd0fb71574722e4ae325beb46bb10772ddde08273</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Diagnostics</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Historical Geology</topic><topic>Paleontology</topic><topic>Soils</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zaidelman, F. R.</creatorcontrib><creatorcontrib>Nikiforova, A. S.</creatorcontrib><creatorcontrib>Stepantsova, L. V.</creatorcontrib><creatorcontrib>Krasin, V. N.</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Moscow University soil science bulletin</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zaidelman, F. R.</au><au>Nikiforova, A. S.</au><au>Stepantsova, L. V.</au><au>Krasin, V. N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Methods for quantitative diagnostics of degree of hydromorphism of chernozem-like soils (based on example of soils of northern Tambov Plain)</atitle><jtitle>Moscow University soil science bulletin</jtitle><stitle>Moscow Univ. Soil Sci. Bull</stitle><date>2012-03-01</date><risdate>2012</risdate><volume>67</volume><issue>1</issue><spage>8</spage><epage>13</epage><pages>8-13</pages><issn>0147-6874</issn><eissn>1934-7928</eissn><abstract>The hydrologic features of chernozem-like soils of the northern Tambov Plain reflect the crystallinity of nonsilicate iron contained in ferromagnetic concretions, as well as the qualitative humus content and other properties. The possibility of using Schwertmann’s criterion and swampiness coefficient in the Zaidel’man-Ogleznev method as diagnostic indices of degree of hydromorphism is shown. A new diagnostic index is suggested, i.e., the hydromorphism criterion (K
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| language | eng |
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| subjects | Diagnostics Earth and Environmental Science Earth Sciences Historical Geology Paleontology Soils |
| title | Methods for quantitative diagnostics of degree of hydromorphism of chernozem-like soils (based on example of soils of northern Tambov Plain) |
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