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Generating policies for sustainable water use in complex scenarios: An integrated land-use and water-use model of Monroe County, Michigan.

机译:在复杂情况下生成可持续用水政策:密歇根州门罗县的土地和水资源综合模型。

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Rapidly declining groundwater levels in Southeast Michigan have raised serious concern since the early 1990s. Hydrological studies suggest that land-use changes have caused this decline. The mechanisms linking land-use and groundwater dynamics are not clear, however. To examine this link, I developed the Water-Use Land-Use Model (WULUM), an agent-based model that serves as an analytical framework to understand how these processes interact to create the observed patterns of resource depletion, and to suggest policies to reverse the process. The agent-based model is empirically based on Monroe County, Michigan, and informed with land-use and survey data and expert knowledge about the case. The land-use component includes the main groundwater extractors in the county: stone quarries, golf courses, farms and households. The groundwater component includes the glacial deposits and the underlying bedrock aquifer. The behavior of water users is defined by simple rules that determine their location and consumption decisions. The dynamics of groundwater are represented through simple diffusion rules between each cell and its immediate neighbors.; Scenario-based simulations provided the medium for exploratory analysis of the integrated land-use/groundwater system. Pre-testing of WULUM highlighted the importance of the glacial recharge rate of the aquifer in determining the regional hydraulic gradient, recommending reexamination of the parameter values cited in literature. Although quarries extract 75 percent of the total withdrawal, simulations showed that eliminating quarry dewatering did not entirely reverse groundwater decline. Urbanization, on the other hand, contributed significantly to long-term decline. Both low-density and high-density zoning restrictions improved aquifer conditions over medium-density development, suggesting a non-linear relationship between intensity of residential use and groundwater levels. Moreover, of all the natural and policy variables, zoning had the greatest influence on urban settlement and therefore on resource consumption. Medium to high values of hydraulic conductivity in some cases reinforced drought conditions by extending the area affected by excess withdrawals, so that land-use policies should discourage residential concentration in those areas.; Thus, while quarries currently affect large areas, expanding suburbanization may lead to regional groundwater depletion in the near future, depending on the spatial distribution and the intensity of development.
机译:自1990年代初以来,密歇根州东南部的地下水位迅速下降,引起了人们的严重关注。水文研究表明,土地利用的变化导致了这种下降。但是,将土地利用与地下水动力学联系起来的机制尚不清楚。为了检查此链接,我开发了水利用土地利用模型(WULUM),这是一种基于代理的模型,该模型用作分析框架,以了解这些过程如何相互作用以创建观察到的资源枯竭模式,并提出政策建议。逆转过程。基于代理的模型以经验为基础,以密歇根州门罗县为基础,并以土地使用和调查数据以及此案的专家知识为依据。土地利用部分包括该县主要的地下水开采者:采石场,高尔夫球场,农场和家庭。地下水成分包括冰川沉积物和下伏的基岩含水层。用水者的行为由确定其位置和用水决策的简单规则定义。地下水的动态通过每个单元格及其直接邻居之间的简单扩散规则来表示。基于方案的模拟为综合土地利用/地下水系统的探索性分析提供了媒介。对WULUM的预测试强调了含水层的冰川补给率在确定区域水力梯度中的重要性,建议重新检查文献中引用的参数值。尽管采石场提取了总取水量的75%,但模拟显示,消除采石场脱水并不能完全逆转地下水的下降。另一方面,城市化为长期下降做出了重要贡献。低密度和高密度分区限制都改善了中密度开发中的含水层条件,这表明住宅使用强度与地下水位之间存在非线性关系。此外,在所有自然和政策变量中,分区对城市居民区和资源消耗的影响最大。在某些情况下,中等至较高的水力传导率会扩大受过度抽水影响的地区,从而加剧干旱状况,因此土地使用政策应阻止这些地区的居民集中。因此,尽管采石场目前影响大片地区,但郊区化的扩大可能会在不久的将来导致区域地下水枯竭,这取决于空间分布和发展强度。

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