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首页> 外文期刊>Journal of the Indian Society of Soil Science >Soil Loss Tolerance Limits for Different Physiographic Regions of Odisha
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Soil Loss Tolerance Limits for Different Physiographic Regions of Odisha

机译:奥里萨邦不同生理区域的土壤流失耐受极限

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摘要

The state of Odisha is severely affected by water erosion induced land degradation due to its hilly and undulating terrain and unsustainable land management practices. Ensuring sustainable development of the state needs appropriate land use plan taking into account the heterogeneity in soil and land resources. In this study, the maximum permissible soil loss rates (T’ value) were computed for 159 mapping units of Odisha by integrating most sensitive soil indicators such as infiltration rate, bulk density, water stable aggregate, organic carbon and fertility status to assess soil quality governing soil resistibility to erosion. For each mapping unit, indicator soil attribute values were quantitatively expressed in 0 to I scale and an aggregate scorewas computed from the attribute scores and the corresponding weights. The results suggested a wide difference in the T’ value among the regions and mapping units, with values varying from 2.5 to 12.5 Mg ha~(-1) yr~(-1). About 45% of total area of the state has a T’ value of 10 Mg ha~(-1) yr~(-1)and 32% having T’ value of 7.5 Mg ha ' yr'. In general, the southern, northern and western regions of the state have a lower T’ values than the coastal plains and delta region. Major chunk of area under Eastern Ghats, Garhjat hills, Dandakaranya and Mahanadi basin has T’ < 10.0 Mg ha~(-1) yr~(-1)and can’t afford to lose more than 7.5 Mg ha ' yr' of soil. The information generated shall serve as a useful guide for devising differential conservation and resource use plans on the basis of soil resource potential.
机译:奥里萨邦州由于其丘陵和起伏的地形以及不可持续的土地管理做法而受到水蚀引起的土地退化的严重影响。考虑到土壤和土地资源的异质性,确保国家的可持续发展需要适当的土地利用计划。在这项研究中,通过整合最敏感的土壤指标(如入渗率,容重,水稳定集料,有机碳和肥力状况)来评估土壤质量,从而计算出奥里萨邦159个测绘单位的最大允许土壤流失率(T'值)控制土壤的抗侵蚀能力。对于每个测绘单元,指标土壤属性值以0到I的比例定量表示,并根据属性得分和相应的权重计算出总得分。结果表明,区域和制图单位之间的T'值差异很大,其值介于2.5至12.5 Mg ha〜(-1)yr〜(-1)之间。该州总面积的45%的T'值为10 Mg ha〜(-1)yr〜(-1),32%的T'值为7.5 Mg ha'yr'。通常,该州的南部,北部和西部地区的T'值低于沿海平原和三角洲地区。东高止山脉,加尔贾特山丘,Dandakaranya和Mahanadi盆地下的大部分土地的T'<10.0 Mg ha〜(-1)yr〜(-1),土壤损失不超过7.5 Mg ha'yr 。所产生的信息将为根据土壤资源潜力制定差异保护和资源利用计划提供有用的指导。

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