<mods:mods version="3.3" xsi:schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-3.xsd" xmlns:mods="http://www.loc.gov/mods/v3" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"><mods:titleInfo><mods:title>Phosphate Buffering Capacity and Supply Parameters Affecting Phosphorus Availability in Vertisols</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">S</mods:namePart><mods:namePart type="family">Shailaja</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">K L</mods:namePart><mods:namePart type="family">Sahrawat</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>Phosphorus availability to plants has been variously&#13;
correlated with the soil P supply factors of quantity,&#13;
intensity and buffering capacity. The underlying&#13;
cause of the differing importance of quantity,&#13;
intensity or buffer capacity to P availability is&#13;
probably the relative effect of these factors on the&#13;
diffusion of P. Phosphorus is primarily transported to&#13;
the root surface through the process of diffusion (Wild&#13;
1981). Olsen and Watanabe (1963) estimated on the&#13;
concentration ofP in the soil solution (intensity), the&#13;
ability of the soil to replenish solution P (i.e. buffer&#13;
capacity and the diffusion coefficient ofP in soil).&#13;
</mods:abstract><mods:classification authority="lcc">Soil Science</mods:classification><mods:classification authority="lcc">Fertilizer Applications</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">1994</mods:dateIssued></mods:originInfo><mods:originInfo><mods:publisher>Indian Sociely of Soii Science</mods:publisher></mods:originInfo><mods:genre>Article</mods:genre></mods:mods>