土壤异质性:印度南部两个不同AESR土壤的比较评估

C. M
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摘要

对来自印度南部两个邦的两个农业生态分区(AESU和AESR)土壤的性质和特征进行了比较研究。利用sentinel-2卫星数据、谷歌图像和top sheet,在AESU和AESR中进行了详细的土壤调查。比较了高地和低地主要土壤的异质性。结果表明,土壤AESU和AESR的性质具有较高的异质性。气候条件(AESU中的热带潮湿地区和AESR中的半干旱条件)、地理条件(AESR中的山谷平原到平缓、非常平缓、中等、陡峭和非常陡峭的斜坡,在AESR中变为平缓和非常平缓的斜坡)、地质条件(AESR中的charnockite和花岗岩片麻岩,而AESR中的花岗岩片麻岩)、土地利用(AESR中的橡胶、水稻、椰子和稻谷、芒果、木豆、花生)、土壤分类(AESR中为Alfisols和ineptisols, AESR中为Alfisols和ineptisols)和土地能力(AESR中必须采取水土保持措施,而AESR中边坡可通过农艺管理措施进行管理)。土壤在质地(AESU中为粘土、砂质粘土和粘土壤土,而AESR中为砂质粘土壤土到砂质壤土)、稠度和深度(AESU中为浅至极深土层,AESR中为浅至深土层)上存在差异。粘土含量为32.9 ~ 63.5%,砂含量为52.1 ~ 72.1%。土壤酸度(强酸到强酸)是AESU的主要问题(氢和铝的饱和),而AESR的主要问题是微酸性到中性和微碱性。AESU中有机碳含量最高(25.9 gkg-1),而AESR中有机碳含量最高(10.0 gkg-1)。AESR的碱基饱和度为75% ~ 100%。碳酸钙当量在AESR中是5%,在AESU中不是问题。AESR中CEC较低(12 cmol (p +) kg-1)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil heterogeneity: A comparative assessment of soils from two different AESR, southern India
A comparative study was carried out to assess the nature and characteristics of soils from two agro-ecological sub regions (AESU and AESR) from two states of South India. Using sentinel-2 satellite data, google imagery and top sheet, a detailed soil survey was taken up in AESU and AESR. Major soils from upland as well as from lowlands were compared to assess the soils heterogeneity. Results showed that there was a high heterogeneity between properties of soils AESU and AESR. Variability existed in climatic conditions (tropical humid region in AESU and semiarid condition in AESR), physiographic (valley plain to gently, very gently, moderate, steep and very steep slopes in AESU and levelled to gently and very gently slopes in AESR ), geology (charnockite and granite gneiss in AESU whereas granite gneiss in AESR), land use (rubber, paddy, coconut in AESU and paddy, mango, pigeon pea, groundnut in AESR), soil classification (Ultisols and Alfisols in AESU whereas Alfisols and Inceptisols in AESR) and land capability (soil and water conservation measures must in AESU and slope was manageable with agronomic management practices in AESR). Soils varied in texture (clay, sandy clay and clay loam in AESU whereas sandy clay loam to sandy loam in AESR), consistency and depth of soils (shallow to very deep in AESU and shallow to deep in AESR). Clay content (32.9 to 63.5%) was dominant fraction in AESU whereas sand (52.1 to 72.1%) was in AESR. Soil acidity (strongly acid to very strongly acid) was a major problem (both hydrogen and aluminium saturation) in AESU whereas slightly acidic to neutral and slightly alkaline in AESR. Organic carbon content was high (up to 25.9 gkg-1) in AESU whereas it was up to 10.0 gkg-1 in AESR. Base saturation was <35% in AESU and >75% up to 100% in AESR. Calcium carbonate equivalent is >5% in AESR and not a problem in AESU. CEC was low (<12 cmol (p+) kg–1) in AESU and good (>12 cmol (p +) kg–1) in AESR.
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