首页> 外文期刊>Ambio: A Journal of the Human Environment >Saltwater Intrusion in the Laizhou Gulf, Shandong Province, China: Causes and Its Impact on Coastal Areas
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Saltwater Intrusion in the Laizhou Gulf, Shandong Province, China: Causes and Its Impact on Coastal Areas

机译:中国山东莱州湾的海水入侵:成因及其对沿海地区的影响

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摘要

Saltwater intrusion or encroachment is a major environmental geological hazard, which is defined as the migration of salt water into freshwater aquifers under the influence of groundwater development (1). Saltwater intrusion becomes a problem in coastal areas where freshwater aquifers are hydraulically connected with seawater. The salinization of the freshwater resources has seriously impeded the development of agriculture and industry and the improvement of the peoples' living standards in these areas. In the mid-1980s, the overexploitation of groundwater exacerbated the saltwater intrusion, and the rate of intrusion continues to increase steadily (2). The Laizhou Gulf, located in Shandong Province of China, is one of the places experiencing serious saltwater intrusion (Fig. 1), Although many studies have focused on groundwater hydro-chemical characteristics (3), causes and prevention countermeasures (4), and sea-water intrusion disaster (5) in the Laizhou Gulf, causes and impacts in the area of saltwater intrusion have received little attention. The objective of this study is the analysis of the causes of saltwater intrusion and its impact on the coastal areas of the Laizhou Gulf. The study area (36 deg 51 min-37 deg 30 min N and 118 deg 38 min-119 deg 36 min E) is located in the northern part of the southern coastal plain of the Laizhou Gulf, Shandong Province, China, with an area of 3772 km~2 (Fig. 2). In the study area, the average annual temperature is 11.5-13 deg C, and the average annual precipitation is 628.6 mm; 70-80 percent of the year's total precipitation comes during June to August. The average annual evaporation is about 1640 mm, chiefly during April to June. The land surface of the study area slopes gently from south to north and is made up of an alluvial and diluvial plain, an alluvial and marine plain, and a marine plain; these are distributed from south to north, respectively. Accordingly, the study area is classified into three type zones from south to north: a freshwater zone with an area of 1158 km~2; a fresh- and saltwater zone with an area of 525 km~2; and a saltwater zone with an area of 2089 km~2.
机译:盐水入侵或侵占是主要的环境地质危害,定义为在地下水开发的影响下盐水向淡水含水层中的迁移(1)。在淡水含水层与海水水力相连的沿海地区,咸水入侵成为一个问题。淡水资源的盐碱化严重阻碍了农业和工业的发展以及这些地区人民生活水平的提高。在1980年代中期,对地下水的过度开采加剧了咸水的入侵,入侵速度持续稳步增加(2)。位于中国山东省的莱州湾是遭受严重海水入侵的地方之一(图1),尽管许多研究集中在地下水的水化学特征(3),成因和预防对策(4),以及莱州湾的海水入侵灾害(5),咸水入侵地区的成因和影响很少引起关注。本研究的目的是分析盐水入侵的原因及其对莱州湾沿海地区的影响。研究区域(北纬36度51分至37度30分钟,东经118度38分至119度36分钟)位于中国山东省莱州湾南部沿海平原的北部, 3772 km〜2(图2)。在研究区,年平均气温为11.5-13摄氏度,年平均降水量为628.6毫米。年总降雨量的70-80%是在6月至8月之间。年平均蒸发量约为1640毫米,主要在4月至6月。研究区的陆地表面由南向北平缓倾斜,由冲积平原和冲积平原,冲积和海洋平原以及海洋平原组成。这些分别从南到北分布。据此,研究区从南到北分为三类:一类为1158 km〜2的淡水区;另一类为1158 km〜2的淡水区。面积525 km〜2的淡水和咸水区;咸水区面积2089 km〜2。

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