沙特阿拉伯Al-Jouf地区灌区水资源管理中地下水盐度监测

A. Al-Naeem
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引用次数: 10

摘要

地下水含盐量是制约沙特阿拉伯可持续灌溉农业的重要因素。地下水总盐度取决于含水层地质及其化学特征。本研究的主要目的是监测沙特阿拉伯Al-Jouf地区灌区的地下水盐度,以便进行水资源管理。在全区随机抽取小、中、大型农场共采集水样117份。对水样进行了主要的阳离子和阴离子分析。全区地下水总盐度小于1000 mg LG1,属于中高盐度和中高碱度水。主要阳离子和阴离子之间的相互作用关系很差。EC与SAR的关系很差(R2 = 0.038)。地下水中约91%为氯化钠型水,其余9%为硫酸钠型水。简单SAR与计算SAR之间的相关性非常强(R2 = 0.988和0.983)。结果表明,淡水入侵对地下水含水层有补充作用。总之,为了提高水的利用效率,需要改进水管理做法,如应用淋溶要求,采用改进的灌溉方法(滴灌和地下灌溉)和适当的作物选择,以提高该地区的农业产量。
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Monitoring of Groundwater Salinity for Water Resources Management in Irrigated Areas of Al-Jouf Region, Saudi Arabia
Groundwater salinity is an important limiting factor to sustainable irrigated agriculture in Saudi Arabia. The total groundwater salinity depends on the aquifer geology and its chemical characteristics. The main objective of this study was to monitor groundwater salinity for water resources management in irrigated areas of Al-Jouf Region of Saudi Arabia. A total of 117 water samples were collected from randomly selected small, medium and large agricultural farms from the whole region. The water samples were mainly analyzed for major cation and anions. The total groundwater salinity in less than 1000 mg LG1 in the whole region and falls in the category of medium to high salinity and medium to high sodicity water. Inter-ion relationship is very poor between major cations and anions. The EC and SAR relationship is very poor (R2 = 0.038). About 91% of groundwater is of sodium chloride type waters and the remaining 9% is that of sodium sulfate type water. The relationship between simple SAR and calculated SARs is very strong (R2 = 0.988 and 0.983). The results showed a replenishment of groundwater aquifer with the fresh water intrusion. In conclusion, to achieve higher water use efficiency, improvement water management practices such as application of leaching requirements, adoption of improved irrigation methods (drip and sub-surface irrigation) and proper crop selection need to be followed for increased agricultural production in the region.
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