Please use this identifier to cite or link to this item: http://nopr.niscair.res.in/handle/123456789/44917
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dc.contributor.authorOrhan, Dengiz-
dc.contributor.authorHüseyin, Şenol-
dc.date.accessioned2018-08-29T08:52:06Z-
dc.date.available2018-08-29T08:52:06Z-
dc.date.issued2018-09-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/44917-
dc.description1809-1820en_US
dc.description.abstractFour soil toposequences served as the basis to calculate the accumulation of soil organic matter, transformation of pedogenic Fe and Al and net losses of the main elements (Ca, Mg, K, Na, Fe, Al, Mn and Si) by means of mass-balance calculations. Elemental losses due to deglaciation and exposure to the weathering environment were calculated. These mass balance calculations indicate that extensive mineral weathering resulted in significant leaching losses of Si, major base cations, and Al (particularly from the upper horizons). Dominant duration identified with mass-balance analysis include desilication and loss of bases.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.47(09) [September 2018]en_US
dc.subjectMass-balanceen_US
dc.subjectSoil formationen_US
dc.subjectToposequenceen_US
dc.subjectXRD of clay fractionen_US
dc.titleEffect of toposequences on geochemical mass balance and clay mineral formation in soils developed on basalt parent material under subhumid climate conditionen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.47(09) [September 2018]

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