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首页> 外文期刊>Journal of the Indian Society of Soil Science >Characterization and Classification of Salt Affected Soils in Mula Command Area of Ahmednagar District, Maharashtra
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Characterization and Classification of Salt Affected Soils in Mula Command Area of Ahmednagar District, Maharashtra

机译:马哈拉施特拉邦艾哈迈德纳加尔地区穆拉指挥区盐碱土的特征与分类

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Soil salinity/sodicity is one of the most serious forms of soil quality degradation affecting approximately 10% of the total land surface of the globe. The problem occurs in varying intensities in more than 120 countries and is more prominently witnessed in the arid and semi-arid areas (Yadav 1993). In semi-arid and arid regions, irrigation induced problems of water-logging, secondary salinization and sodication goes hand in hand. These problems pose a great threat to the sustainable productivity. Nearly 10-12% of shrink-swell soils under command of Mula, Pravara, Godavari, Dhom, Girna, Purna, Jayakwadi, Nira, Krishna, Mutha and several such major and minor irrigation projects have turned into saline and sodic Vertisols (Varade et al. 1985). India covers an area of salt affected soils to the tune of 13.5 million hectare (Mha). In Maharashtra state about 0.54 Mha of black soils are initially reported to be salt affected which has increased to 1.06 Mha and is about 3.4% of geographical area (Gaikwadand Challa 1996). The soils of Mula command area in distributory No.2 turned to highly saline after 35 years of introduction of canal irrigation. Kharche and Pharande (2010) reported that about 65% area in the Mula command was affected by salinity and sodicity, out of which 36% area was found to be sodic, while 29% was saline-sodic. Therefore, it is necessary to characterize and classify the soils in distributory No. 2 of Mula command area after lapse of 35 years. The present investigation was therefore, planned in order to develop the database on physical and chemical properties of soil as affected by salinity and sodicity in Mula command area of Ahmednagar district.
机译:土壤盐度/碱度是最严重的土壤质量退化形式之一,影响了全球约10%的陆地表面。这个问题在120多个国家以不同的强度发生,在干旱和半干旱地区尤为明显(Yadav 1993)。在半干旱和干旱地区,灌溉引起的涝灾,次生盐渍化和加盐问题并存。这些问题对可持续生产力构成了巨大威胁。在穆拉,普拉瓦拉,戈达瓦里,多姆,吉尔纳,普尔纳,贾亚克瓦迪,尼拉,克里希纳,穆塔和其他几个大型和小型灌溉项目的控制下,将近10-12%的收缩膨胀土壤变成了盐碱和苏打粉饰(Varade等(1985)。印度的盐碱土壤覆盖面积达1,350万公顷(Mha)。在马哈拉施特拉邦,最初据报道约有0.54 Mha的黑色土壤受到盐的影响,现已增加到1.06 Mha,约占地理面积的3.4%(Gaikwadand Challa 1996)。引入运河灌溉35年后,2号分布地区的穆拉指挥区的土壤变成了高盐分。 Kharche和Pharande(2010)报告说,穆拉命令中约有65%的地区受盐度和苏打水的影响,其中36%的地区为苏打水,而29%的地区为苏打水。因此,经过35年后,有必要对穆拉指挥区2号分布区的土壤进行表征和分类。因此,计划进行本次调查,以开发艾哈迈德纳加尔地区穆拉指挥区受盐碱度影响的土壤理化特性数据库。

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