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Influence of irrigation water on black soils in Amravati district, Maharashtra

机译:马哈拉施特拉邦阿姆拉瓦蒂地区灌溉水对黑土的影响

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摘要

In view of earlier reports on the occurrence of salt-affected shrink-swell soils in the Purna valley areas in Amravati district of Maharashtra, the present study was carried out to assess the current nature and extent of soil degradation due to use of irrigation water. Results indicate that the irrigation water used to raise agricultural crops in Amravati, Bhatkuli, Warud and Daryapur tehsils contains enough soluble Na-ions and residual sodium carbonate as the water belongs to C4S2 and C4S1 class of the United States Salinity Laboratory. The anthropogenic activities by introducing irrigation have caused severe drainage problem in the shrink-swell soils of the district, which are highly clayey and smectitic that have inherent low permeability. Only exception is the better drained soils of Warud tehsil, which are endowed with Ca-zeolite that help to ward off the ill effects of irrigation. The study thus suggests that continuing the present anthropogenic activities might render the soils unsuitable for agricultural production in the future. In contrast, the soils which are not irrigated do not suffer from any serious degradation in terms of high exchangeable Na (ESP) and low saturated hydraulic conductivity (sHC), suggesting that it would be prudent to encourage rainfed agriculture in the district under improved management practices.
机译:鉴于较早的关于在马哈拉施特拉邦Amravati区Purna山谷地区发生盐影响的收缩膨胀土壤的报道,本研究旨在评估由于灌溉水导致的土壤退化的现状和程度。结果表明,用于种植Amravati,Bhatkuli,Warud和Daryapur tehsils的农作物的灌溉水含有足够的可溶性Na离子和残留的碳酸钠,因为该水属于美国盐度实验室的C4S2和C4S1类。引入灌溉的人为活动在该地区的膨胀膨胀土壤中引起了严重的排水问题,这些土壤具有高黏性和近渗性,固有渗透性较低。唯一的例外是Warud tehsil排水良好的土壤,这些土壤拥有钙沸石,有助于抵御灌溉的不良影响。因此,研究表明,继续目前的人为活动可能会使土壤不适合将来的农业生产。相比之下,未灌溉的土壤在高交换性钠(ESP)和低饱和导水率(sHC)方面并未遭受任何严重的退化,这表明在管理完善的地区鼓励雨养农业是谨慎的做法。实践。

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