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Morphological, physico-chemical and mineralogical characteristics of some soils of semiarid submoist lower Kandi zone of Punjab

By: Material type: TextTextSubject(s): Summary: Tehe climate of the are is Semiarid (submoist) and less hot qualiifying it for ustic soil moisture rfegime and hyperthermic temperature regime. The major landscaepe elelT1ents recognized in the area were shoulder slope,foot slope, upper piedmont plain, an
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Theses/ Dissertation Theses/ Dissertation Mohinder Singh Randhawa Library Not for loan 222196
Theses/ Dissertation Theses/ Dissertation Mohinder Singh Randhawa Library Not for loan 222197

Tehe climate of the are is Semiarid (submoist) and less hot qualiifying it for ustic soil moisture rfegime and hyperthermic temperature regime. The major landscaepe elelT1ents recognized in the area were shoulder slope,foot slope, upper piedmont plain, an

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