干旱与土地利用变化评价:对乌尔米亚湖北部Shabestar盆地地下水水质的影响

Desert Pub Date : 2018-01-01 DOI:10.22059/JDESERT.2018.66344
M. Ranjpisheh, M. K. Reihan, G. Zehtabian, H. Khosravi
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引用次数: 10

摘要

在干旱和半干旱地区,地下水水质管理非常重要。利用TM、ETM和OLI遥感卫星影像,分析了1990年、2007年和2015年Shabestar流域土地利用变化对地下水水质的影响。通过对图像的处理和分析,将流域划分为牧场、裸地、农业、园林和住宅5类土地利用类型。利用3年、5年和7年的激励平均值来确定降水变化趋势和确定湿润期和干旱期。利用地质统计学方法绘制了2002 - 2012年10年间40口井的EC、SAR、TH、Cl和Na等定性参数的分区图,以评价地下水水质的变化。激励平均图结果表明,1997 ~ 2003年第一期由于降水不足,出现了干旱,其中1999年干旱最为严重。总体而言,地下水质量在这一时期有所改善。第一期(2002-2005年)与干旱期重合,水质较差;第二期和第三期(2006-2009年和2010-2012年)与湿润期重合,水质有所改善。位于乌尔米湖附近的南部和西部水质参数数量增加,这些地区的水不适合耕种和饮用。这可能是由于地下水的过度使用受到该地区土地利用变化的影响。
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Assessment of drought and landuse changes: Impacts on groundwater quality in Shabestar basin, North of Lake Urmia
Management of groundwater quality is very important in arid and semi-arid areas. In this study, satellite images from TM, ETM and OLI sensors were used to evaluate the impacts of land use changes on groundwater quality for 1990, 2007 and 2015 in Shabestar basin. After processing and analyzing images, the basin was classified into five land use classes including pasture, bare land, farming, garden and residential. Motivate averages of 3, 5 and 7 years were used to determine precipitation changes trends and identifying wet and drought periods.  Zoning maps of qualitative parameters including EC, SAR, TH, Cl and Na for 40 wells in a decade (2002 to 2012) were plotted using geostatistical methods to evaluate changes in groundwater quality. The obtained results from motivating average graph showed that drought was occurred during the first period 1997 to 2003 due to lack of rainfall, the worst drought was occurred in year 1999. Overall, the quality of groundwater was improving over the period. So that water quality was low in the first period (2002-2005) due to coinciding with the drought period and water quality was improving due to coinciding with wet periods in the second and third period (2006-2009 and 2010-2012). The amount of water quality parameters has increased in the southern and western parts of the region where located in the vicinity of Lake Urmia and water in these areas aren’t suitable for farming and drinking. It can be due to overuse of groundwater affected by land use changes in this parts of the region.
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