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Groundwater Regulation and the Development of Alternative Source Waters to Prevent Subsidence, Houston Region, Texas, USA

机译:地下水监管与开发替代源水域,以防止沉降,休斯顿地区,德克萨斯州,美国

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Since the development of the coastal areas near present-day Houston, Texas, USA, subsidence has been a significant public policy concern. Subsidence in this area is caused by the extraction of groundwater from the Coastal Lowlands aquifer system, locally referred to as the Gulf Coast Aquifer. Concerns associated with subsidence in the Houston area include coastal inundation from storm surge, inland flooding, and critical infrastructure damage. The Houston area receives about 126 cm of precipitation each year, making flooding a critical issue in the region. The Houston area is the 4th largest city in the United States with a population of about 6.89 million (2017) and has a total water demand of about 4 Mm~3 per day (2017). In the 1950s the City of Houston began the development of several reservoirs to provide water for the rapidly growing city. In 1975, following decades of subsidence totaling over 3 m, the Harris-Galveston Subsidence District (District) began regulating the use of groundwater and shifting the primary water supply for the region from groundwater to treated surface water to cease on-going and prevent future subsidence. Leveraging the alternative resources developed by the City of Houston in the 1950s, the District's regulatory framework focuses on spatial prioritization and the systematic conversion to alternative source waters. The District's regulatory plan includes three planning areas. Currently, the regional water authorities and the City of Houston are developing nearly five billion dollars (USD) in infrastructure to produce and deliver an additional 1.2 Mm~3 per day of treated surface water to Houston and the surrounding communities. Resource development, public engagement, and political foresight have resulted in a reasonable approach to shift source waters and implement a plan to dramatically reduce and stop subsidence in the region. Figure 2 presents subsidence rates (2017) by regulatory area. Results show that the implementation of the reg
机译:自从当今休斯顿附近的沿海地区的发展以来,美国德克萨斯州,沉降是一项重大的公共政策问题。该地区的沉降是由沿海低地含水层系统的地下水的提取引起的,作为墨西哥湾沿岸含水层。与休斯顿地区沉降有关的担忧包括风暴浪涌,内陆洪水和关键基础设施损坏的沿海泛滥。休斯顿地区每年收到约126厘米的降水量,使该地区的批判问题造成洪水。休斯顿地区是美国第四大城市,人口约689万(2017年),每天约为4毫米〜3的总需水量(2017年)。在20世纪50年代,休斯敦市开始开发几个水库,为快速增长的城市提供水。 1975年,在哈里斯 - 加尔维斯顿沉降区(区)超过3米的几十年沉降,开始调节地下水的使用,从地下水到地下水处理地表水以停止,防止未来,防止未来沉降。该地区的监管框架利用休斯顿市开发的替代资源侧重于空间优先级和替代源水域的系统转换。该地区的监管计划包括三个规划领域。目前,区域水当局和休斯顿市正在开发近50亿美元(美元)的基础设施,以生产,每天额外的1.2毫米〜3次处理的地表水到休斯顿及周边社区。资源开发,公众参与和政治远见导致了一种合理的方法来改变源水域,并实施计划,以大大减少该地区的沉降。图2介绍了监管区域的次息(2017年)。结果表明,瑞典的实施

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