首页> 外文期刊>Journal of the Indian Society of Soil Science >Characterization of Some Salt Affected Soils and Poor Quality Waters of Kaithal District in Central Haryana for Reclamation and Management
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Characterization of Some Salt Affected Soils and Poor Quality Waters of Kaithal District in Central Haryana for Reclamation and Management

机译:哈里亚纳中部哈里亚地区一些盐影响土壤和贫困品质的特征

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摘要

Salt affected soils and poor quality ground waters are primary constraints for sustainable agriculture in arid and semi-arid climatic zones of central Haryana (Yadav 2003). High evaporation during the dry season and lack of good quality water for irrigation caused salt accumulation in soil profiles. The use of poor quality ground water for irrigation has increased salt build-up in soil profiles and caused reduced productivity. Naturally, salts are drained from the Himalayas and Siwalik through rivers/streams and are accumulated at the alluvial plains (Sidhu et al. 1995). The lack of adequate internal drainage in lower topographic regions prompted soil salinization (Bhargava et al. 1980). Canal irrigation in undrained areas has caused waterlogging, formation of high water table and secondary salinization in soils. Due to dynamic nature, these soils showed variable extent during dry and wet seasons.
机译:盐受影响的土壤和质量差的地面水域是中央哈里亚纳邦干旱和半干旱气候区的可持续农业的主要限制(Yadav 2003)。 干燥季节期间的高蒸发,缺乏灌溉良好的水,导致土壤剖面盐积累。 使用差的灌溉质量差,在土壤型材上增加了盐堆积,提高了生产率。 当然,盐通过河流/溪流从喜马拉雅山脉和Siwalik排出,并积累在冲积平原(Sidhu等人1995)。 较低地形区域缺乏足够的内部引流促使土壤盐渍化(Bhargava等,1980)。 在不介绍地区的运河灌溉导致涝渍,在土壤中形成高水位和二次盐渍化。 由于动态性质,这些土壤在干燥和潮湿的季节显示了可变程度。

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    Central Soil Salinity Research Institute Zarifa Farm Kachhwa Road Karnal 132 001 Haryana;

    Central Soil Salinity Research Institute Zarifa Farm Kachhwa Road Karnal 132 001 Haryana;

    Central Soil Salinity Research Institute Zarifa Farm Kachhwa Road Karnal 132 001 Haryana;

    Central Soil Salinity Research Institute Zarifa Farm Kachhwa Road Karnal 132 001 Haryana;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 土壤学;
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