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        <dc:title>Characterization and Classification of Soils from Three&#13;
Agro-climatic Zones of Belgavi District, Karnataka</dc:title>
        <dc:creator>Prabhavati, K</dc:creator>
        <dc:creator>Dasog, G S</dc:creator>
        <dc:creator>Sahrawat, K L</dc:creator>
        <dc:creator>Patil, P L</dc:creator>
        <dc:creator>Wani, S P</dc:creator>
        <dc:subject>Soil</dc:subject>
        <dc:subject>Karnataka</dc:subject>
        <dc:subject>Watershed Management</dc:subject>
        <dc:description>Belgavi district in Karnataka is characterized by three contrasting agro-climatic zones viz., a relatively dry&#13;
semi-arid northern dry zone (Zone-3) with low rainfall, a somewhat higher rainfall area termed transitional&#13;
zone (Zone-8) nestling between the Western Ghats and Eastern Plains, and a heavy rainfall area comprising&#13;
part of Western Ghats called hilly zone (Zone-9). This situation provided an opportunity to compare the&#13;
properties of pedons occurring in these agro-climatic zones. Nine pedons, three each from the three microwatersheds&#13;
viz., Yadawad (Zone-3), Hukkeri (Zone-8) and Khanapur (Zone-9) were characterized for their&#13;
morphological, physical and chemical properties with an objective of comparing their properties which&#13;
have an implication on their use and behaviour. Pedons from Yadawad micro-watershed (Zone-3) were&#13;
deep, alkaline, calcareous and contained considerable amount of salts and are rich in clay content. The&#13;
pedons of Hukkeri micro-watershed (Zone-8) were shallow to moderately deep, neutral, non-calcareous&#13;
and contained low amount of salts and are somewhat coarse textured. Despite similar parent rock (basalt) in&#13;
these two micro-watersheds, the variation in depth and texture are a direct result of erosion and deposition&#13;
due to topographic variations. The pedons from Khanapur micro-watershed (Zone-9) were acidic, highly&#13;
leached, and moderately fine textured. The variation in the soil properties of soils of Khanapur watershed&#13;
sharply contrasted with soils of both Yadawad and Hukkeri watersheds due to high rainfall at the former&#13;
compared to the latter. The soils of Yadawad micro-watershed classify as Typic Calciusterts, those of&#13;
Hukkeri micro-watershed as Lithic and Typic Ustorthents and the soils of Khanapur micro-watershed as&#13;
Oxic Dystrustepts and Kanhaplic Haplustalfs reflecting the leaching regime and erosion of sediments&#13;
during soil formation.</dc:description>
        <dc:publisher>Indian Society of Soil Science</dc:publisher>
        <dc:date>2017</dc:date>
        <dc:type>Article</dc:type>
        <dc:type>PeerReviewed</dc:type>
        <dc:format>application/pdf</dc:format>
        <dc:language>en</dc:language>
        <dc:identifier>http://oar.icrisat.org/9995/1/Prabhavati%20et%20al%202017.pdf</dc:identifier>
        <dc:identifier>  Prabhavati, K and Dasog, G S and Sahrawat, K L and Patil, P L and Wani, S P  (2017) Characterization and Classification of Soils from Three Agro-climatic Zones of Belgavi District, Karnataka.  Journal of the Indian Society of Soil Science, 65 (1).  pp. 1-9.  ISSN 0974-0228     </dc:identifier>
        <dc:relation>http://doi.org/10.5958/0974-0228.2017.00001.9</dc:relation>
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