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The role of groundwater in the management of water resources in the World

机译:地下水在世界水资源管理中的作用

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Groundwater forms about 98% of all the fresh liquid water available in the World. Even so, groundwater is the forgotten and most ignored part of the water cycle. Any time a drop of water infiltrates into the soil, it enters an occult world where still today many mysteries need to be solved. Studies can sometimes prove the journey of water under the soil, from the infiltration point to a discharge point, but it is practically impossible to know the exact path of this drop along the subterranean journey. The same is true for groundwater quality. The infiltrating water begins to interact chemically with the soil particles immediately it enters the soil, within the unsaturated zone. When it enters the saturated zone (aquifer) it interacts with the rock and weathered materials, dissolving minerals, interchanging ions, depositing in other places previously dissolved substances, in a permanent change that includes interaction with human activities, be it capture by a pump in a well or the contamination caused by infiltrating residual water from agriculture or a sewage system.
机译:地下水形成了世界上所有新鲜液体用水的98%。即便如此,地下水是被遗忘的和最忽略的水循环部分。随着一滴水渗透到土壤中,它进入了许多奥秘需要解决的隐匿世界。研究有时可以证明土壤下的水之旅,从渗透点到排放点,但实际上是不可能知道这一滴水的确切路径沿着地下旅程。地下水质量也是如此。渗透水开始在化学上与土壤颗粒立即进入不饱和区内的土壤。当它进入饱和区(含水层)时,它与岩石和风化的材料相互作用,溶解矿物质,互换离子,在以前溶解物质的其他地方沉积,包括与人类活动相互作用,以泵捕获通过渗透来自农业或污水系统而引起的井或污染。

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