2003
DOI: 10.1079/sum2003191
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Use of hydraulic conductivity to evaluate the suitability of Vertisols for deep-rooted crops in semiarid parts of central India

Abstract: Detailed morphological, physical, chemical, mineralogical and micromorphological studies were carried out to identify properties that in¯uence the yield of deep-rooted crops in 29 Vertisols of semiarid central India, since existing land evaluation methods are not adequate to explain the yield of cotton obtained by farmers. The studies indicated that among the soil parameters, CaCO 3 in the clay fraction, the exchangeable Ca/Mg ratio, exchangeable sodium percentage (ESP) and saturated hydraulic conductivity (HC… Show more

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Cited by 41 publications
(10 citation statements)
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“…This type of degradation ultimately modifies the soil physical and chemical properties. Such modifications resulting through the regressive pedogenesis 12 restrict the entry of rain water, and reduces the storage and release of soil water 13 . The lack of soil water impairs the possibility of growing both rainy and winter crops in a year, in vast areas especially in black soils of SAT with mean annual rainfall (MAR) <1000 mm (ref.…”
Section: Smith and Powlsonmentioning
confidence: 99%
“…This type of degradation ultimately modifies the soil physical and chemical properties. Such modifications resulting through the regressive pedogenesis 12 restrict the entry of rain water, and reduces the storage and release of soil water 13 . The lack of soil water impairs the possibility of growing both rainy and winter crops in a year, in vast areas especially in black soils of SAT with mean annual rainfall (MAR) <1000 mm (ref.…”
Section: Smith and Powlsonmentioning
confidence: 99%
“…The release of Ca 2+ ions from soil modifiers prevents a rise in pH and ESP and improves the soil hydraulic properties to obliterate the effect of high ESP. As suggested, the lower limit of sodicity at ESP > 40 for soils of the Indo‐Gangetic Plains (IGP) (Abrol and Fireman, 1978), at ESP >5 but <15 for Indian Vertisols (Kadu et al, 2003), or the limit of ESP 6 for Australian soils or >15 for all soil types (Soil Survey Staff, 1999, 2003) appears to be redundant for the zeolitic sodic Vertisols of India. In view of the pedogenetic processes controlling the hydraulic properties of soils mediated through dispersibility, the most important factor for soil degradation (Sumner, 1995), grouping soils on the basis of saturated hydraulic conductivity ( K s ) appears logical.…”
Section: Vertisols and Their Classificationmentioning
confidence: 99%
“…To estimate LGP, 100 mm m -1 water has been used as standard for the deep soils assuming this amount to be the measure of available water after cessation of rains. Later Kadu et al (2003) reported this measure to be an over estimation. This demanded estimation of the LGP to be modified .…”
Section: Methodology To Develop Agro-ecological Sub Regions (Aesrs)mentioning
confidence: 99%