Mapping and characterization of salt-affected and waterlogged soils in the Gangetic plain of central Haryana (India) for reclamation and management

A. Mandal
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引用次数: 20

Abstract

Abstract IRS LISS III Resource SAT data (2005–07) were integrated with ground truth and soil studies for delineation and characterization of salt-affected and waterlogged soils in the Indo-Gangetic plain of central Haryana. The quality appraisal for salty ground water was also conducted prior to its use for irrigation. Such studies are useful for planning reclamation and management of salt-affected soils and poor quality ground water. Strongly sodic soils were easily identified based on the white to yellowish white tones, high spectral and low NDVI values. Waterlogged areas (surface ponding) were detected based on higher absorption in infrared range. Sodic soils with poor quality ground water showed higher reflectance from dry salts during June and freshly precipitated moist salts in March and October. Sodic soils irrigated with normal ground water showed higher cropping density and higher NDVI values. Moderately and slightly sodic soils showed mixed spectral signatures for salt crusts, moderate cropping density and surface wetness. Soil profile studies indicated higher moisture content at sub-surface depths. The presence of iron and manganese mottles indicated the incidences of water stagnation. Soils with high pHs, ESP, and SAR values and showing the dominance of carbonate and bicarbonates of sodium in the saturation extract indicated sodic nature. Significant presence of CaCO3 concretions at 1 m depth, low organic carbon contents, clay illuviation at sub-surface depth are typical features in sodic soil profiles. Water samples with high pH and SAR values and at places high RSC (Residual Sodium Carbonate) content indicated their sodic nature. Gypsum application is recommended for the reclamation of sodic soils and sodic water.
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哈里亚纳邦(印度)中部恒河平原盐渍和涝渍土壤的制图和特征,用于复垦和管理
利用2005 - 2007年的IRS LISS III资源SAT数据与地面实况和土壤研究相结合,对哈里亚纳邦中部印度恒河平原的盐渍和涝渍土壤进行了圈定和表征。咸地下水在用于灌溉前也进行了水质评价。这些研究对规划、开垦和管理受盐影响的土壤和劣质地下水是有用的。强碱化土壤具有白色至黄白色、高光谱和低NDVI特征。利用红外波段的高吸收来探测地表积水区。地下水质量差的钠质土壤在6月表现出较高的干盐反射率,在3月和10月表现出较高的湿盐反射率。正常地下水灌溉的碱土种植密度较高,NDVI值较高。中度和轻度盐碱化土壤表现出盐结、中等种植密度和地表湿度的混合光谱特征。土壤剖面研究表明,地下深度的含水率较高。铁斑和锰斑的存在表明水停滞的发生。ph值、ESP值和SAR值较高的土壤,在饱和萃取物中以碳酸盐和碳酸氢盐为主,表明土壤具有钠性。1 m深度存在大量CaCO3结块,低有机碳含量,次表层深度存在粘土沉积,是盐渍土剖面的典型特征。高pH值和SAR值的水样以及高残余碳酸钠含量的水样显示出其钠性。建议在碱土和碱水的复垦中使用石膏。
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Cogent Geoscience
Cogent Geoscience GEOSCIENCES, MULTIDISCIPLINARY-
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