基于地理空间工具的丹纳斯塔华(曼查尔湖)指挥区水土种植格局研究

A. A. Siyal, Imran Lakhair, M. Babar, Pirah Siyal, G. S. Solangi
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引用次数: 5

摘要

右岸排水渠的排放不仅对曼查尔湖的水生生物构成威胁,而且对利用丹纳斯达华湖水耕作的肥沃农田也有盐碱化的危险。该地区的农业社区对持续使用达纳斯塔河的灌溉用水感到恐惧;他们认为,不断使用这种水会把他们肥沃的土地变成受盐影响的土壤。因此,考虑到Danastar Wah指挥地区农民的担忧,我们开展了一项研究,调查了Manchar湖、RBOD MNV(主要奈良山谷)排水沟和Danastar Wah的水质,并利用2015年Kharif季节的地理参考野外和卫星图像数据检查了该地区的土壤盐度状况。研究结果表明,丹纳斯塔华水的电导率(EC)在1.2 dS/m以下。因此,水适合灌溉的目的。所有水样中Na+、Ca2+ + Mg2+和CO3浓度均在允许范围内,未发现HCO3浓度。在指挥区,粘土质地占主导地位,直至60 cm深度的土壤剖面。该地区正常土壤(非盐碱化)、盐碱化土壤和盐碱化土壤的比例分别为37%、28%和30%;而只有5%的土壤是盐碱化的。棉花作物被确定为主要的Kharif作物,占总指挥面积的13.76%(2844公顷),其次是水稻作物,约占指挥面积的5.21%(1078公顷)。图像分类的总体准确率为90%,kappa系数为0.86。本研究认为,只有在保持充足的土地排水的条件下,达纳斯塔河的水才能在丰收季节用于灌溉。建议在腊季使用Manchar湖、RBOD和Danastar Wah水之前,进行水质分析。地理信息系统(GIS)和遥感(RS)工具可用于曼查尔湖水质的时空监测。
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Study of Soil, Water, and Cropping Pattern in Danastar Wah (Manchar Lake) Command Area Using Geospatial Tools
The effluent water brought by RBOD (Right Bank Outfall Drain) is not only threat to the aquatic life of Manchar Lake but also the fertile agricultural lands which are being cultivated by use of lake water through Danastar Wah are at risk of salinization. The farming community of the area is scary of continual use of irrigation waters received through the Danastar Wah; they are of the view that the constant use of this water will ruin their fertile lands into salt-affected soils. Thus, keeping in view the fears of the farmers of the command area of Danastar Wah, a study was carried out to investigate the water quality of the Manchar Lake, RBOD MNV (Main Nara Valley) drain and Danastar Wah, and to examine soil salinity status of the area using Geo-referenced field and satellite imagery data for Kharif season of the year 2015. The results of the study showed that the EC (Electrical Conductivity) of the Danastar Wah water was below 1.2 dS/m. Thus, the water was suitable for irrigation purpose. In all the water samples, Na+, Ca2+ + Mg2+ and CO3 concentrations were found within the permissible limits, while no concentration of HCO3 was found in any of the water samples. In the command area, clay texture was dominant down to a depth of 60 cm soil profile. In the area about 37, 28, and 30% of the soils were normal (non-saline), saline and sodic, respectively; while only 5% of soils were saline-sodic. The cotton crop was identified as the major Kharif crop, occupying about 13.76% (2,844 ha) of the total command area, followed by rice crop grown on about 5.21% (1,078 ha) of the command area. The overall accuracy of image classification was 90% with a kappa coefficient of 0.86. Based on this study, it can be concluded that the water of the Danastar Wah can be used for irrigation purpose during Kharif season only with the condition that adequate land drainage is maintained. It is also suggested that before using the water of Manchar Lake, RBOD and Danastar Wah for Rabi season, analysis for water quality be conducted. GeoInformatics (GIS and RS) tools can be employed for spatial and temporal monitoring of water quality of the Manchar Lake.
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