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THE PHYSICAL AND ECONOMIC IMPACT OF AQUIFER OVER-EXPLOITATION AT HANGU, CHINA

机译:汉沽含水层过度剥削的身体经济影响

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During the second half of this century, the deep unconsolidated sedimentary aquifer under tlie coastal city of Hangu has been heavily exploited by the local industry, agriculture and domestic users. This has caused large piezometric head reductions and has resulted in significant land subsidence. The proximity of the sea makes this particularly undesirable. In order to better understand the relationship between the groundwater abstraction and tlie aquifer compaction, a computer model of the aquifer system which simulated the settlement was created. The nature of the local geology which included thick, slow-draining, clayey aquitards meant that the compaction was delayed in relation to the reduction in pressure in the more transmissive, sandy layers. The reproduction of this delay required the development of a special model package. The modelling indicated that a significant reduction in abstraction was required to restrict the amount of future subsidence to an acceptable level. In parallel with the specific hydrogeological investigation of subsidence, a wider socio-economic study of aquifer over-exploitation used the Hangu situation as a case study. This concluded that water scarcity threatens future regional development, but that more efficient water allocation and efforts to manage groundwater demand might go some way towards putting water use on a more sustainable footing and reduce the need for supply augmentation.
机译:在本世纪下半叶,tlie海滨城市汉沽下深松散沉积含水层已经深受当地工业,农业和国内用户利用。这已经引发了大规模测压头下降并导致显著地面沉降。海的接近使得这个特别不希望的。为了更好地理解之间的关系的地下水开采和tlie含水层压实,其模拟结算创建的含水层系统的计算机模型。当地的地质的,其中包括厚,缓慢引流的性质,粘土弱透水层意味着压实是相对于在更透射,沙层在压力的降低被延迟。这种延迟的复制需要特殊的模型的开发包。建模表明,在一个抽象减少显著被要求未来下沉量限制到可接受的水平。在与下沉的具体水文地质勘察,地下水过度开采的更广泛的社会经济研究并行使用汉沽情况作为案例研究。这个结论是水资源短缺威胁到未来的区域发展,但更高效的水资源分配和管理地下水需求的努力可能会在某种程度上有助于把水用在更可持续的基础,并减少供应增大的需求。

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