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地下水在关键带科学中的重要性。

The Importance of Groundwater in Critical Zone Science.

机构信息

Hydrologic Science and Engineering Program, Geology and Geological Engineering Department, Colorado School of Mines, Golden, CO, USA.

出版信息

Ground Water. 2022 Jan;60(1):27-34. doi: 10.1111/gwat.13143. Epub 2021 Nov 16.

Abstract

The critical zone (CZ)-from treetops to groundwater-is an increasingly studied part of the earth system, where scientists study interactions between water, air, rock, soil, and life. Groundwater is both a boundary and an essential store in this integrated system, but is often not well considered in part because of the difficulty in accessing it and its slow movement relative to other parts of the system. Here, we describe some fundamental areas where groundwater hydrology is of fundamental importance to CZ science, including sustaining streamflow and vegetation, reacting with minerals to produce dissolved solutes and regolith, and influencing energy fluxes across the land-atmosphere interface. As the timing and type of precipitation change with climate, groundwater may play an even more important role in CZ processes as a sustainable water source for plants and streamflow. Many open questions also exist about the role of CZ processes on groundwater. Many data streams are needed and important to quantifying the integrated response of the CZ to groundwater and vice versa, but long-term data records are often incomplete or discontinued due to limited funding. We argue that the long timescales of processes that involve groundwater necessitate data collection efforts beyond typical federal funding timespans. Sustaining monitoring networks and developing new ones aimed at testing hypotheses related to slow-moving, groundwater-controlled CZ processes should be a scientific priority, and here we outline some open questions that we hope will motivate groundwater scientists to get involved in CZ science.

摘要

从树梢到地下水,关键带(CZ)是地球系统中一个越来越受关注的部分,科学家们在这里研究水、空气、岩石、土壤和生命之间的相互作用。地下水既是这个综合系统的边界,也是其基本的储存库,但由于难以获取以及与系统其他部分相比其运动速度较慢,地下水通常没有得到很好的考虑。在这里,我们描述了一些基本领域,其中地下水水文学对 CZ 科学具有根本重要性,包括维持水流和植被、与矿物质反应产生溶解溶质和表土、以及影响陆地-大气界面的能量通量。随着气候变化,降水的时间和类型发生变化,地下水可能会作为植物和水流的可持续水源,在 CZ 过程中发挥更重要的作用。关于 CZ 过程对地下水的作用,也存在许多悬而未决的问题。许多数据流对于量化 CZ 对地下水的综合响应以及反之亦然都非常重要,但由于资金有限,长期数据记录往往不完整或中断。我们认为,涉及地下水的过程的时间尺度很长,因此需要超出典型联邦资助时间范围的努力来收集数据。维持监测网络并开发新的监测网络,旨在测试与缓慢移动、受地下水控制的 CZ 过程相关的假设,应该是科学优先事项,在这里我们概述了一些悬而未决的问题,我们希望这些问题能够激发地下水科学家参与 CZ 科学。

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