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排序方式: 共有1311条查询结果,搜索用时 109 毫秒
91.
渭干河灌区的水土环境及水文地质条件在克孜尔水库建成后发生了一定的变化,本文结合灌区12年来的水盐监测资料,对灌区地下水的埋深变化规律、水质演变趋势、灌区的排水效果及目前存在的问题进行了分析与探讨,并为今后灌区排水措施和保持水土环境的良性发展提出了建议. 相似文献
92.
Abstract The Minshan Mountain and adjacent region are the major continental escarpments along the eastern Tibetan Plateau. The Minjiang drainage basin is located within the plateau margin adjacent to the Sichuan Basin. Based on the analysis of the digital elevation model (DEM) acquired by the Shuttle Radar Topography Mission (SRTM), we know that the Minjiang drainage basin has distinct geomorphic characteristics. The regular increasing of local topographic relief from north to south is a result of the Quaternary sediment deposition within the plateau and the holistic uplift of the eastern margin of the Tibetan Plateau versus the Sichuan Basin. Results from DEM-determined Minjiang drainage sub-basins and channel profiles show that the tributaries on the opposite sides are asymmetric. Lower perimeter and area of drainage sub-basins, total channel length and bifurcation ratio within eastern flank along the Minjiang mainstream are the result of the Quaternary differential uplift of the Minshan Mountain region. Shorter stream lengths and lower bifurcation ratio might be the indications of the undergrowth and newborn features of these eastern streams, which are also representative for the eastern uplift of the Minshan Mountain. 相似文献
93.
鉴于目前入河排污口流量测验手段不足,尝试采用测试电导率方法进行排污口流量测量,并与常规流量测验方法容量法进行比对,试验证实本方法简便易行,适应性强,可以在实际工作中推广应用。 相似文献
94.
在河流中开辟生化反应区、直接布设仿生填料净化河流微污染水体可以达到改善入湖水质、减少投资、降低能源消耗的目的。但在河道内直接布设填料势必会对河流的水动力条件及其河流原有的使用功能造成一定的影响。从填料给水流带来的阻力、流速及糙率变化等方面进行河道内直接布设生物填料对河流水动力条件的影响试验分析。结果表明,由于河道流速不大(属于缓流水体),9根/m2的填料布设密度对水流的扰动作用程度不高,填料段的糙率仅为无填料段糙率的1.08倍,不会对河道的泄水能力造成影响。 相似文献
95.
顾及密度差异的河系简化 总被引:7,自引:2,他引:7
河系简化是地图综合中经常需要处理的任务,其难点主要在于依据上下文环境对河流进行结构化选取,以保持河网密度差异等宏观特征。提出一种新的河流等级规则,依据河流的各级支流的数量确定河流的等级,以反映河流的密度差异;设计一种结合河流等级、长度与所在层次的综合指标进行河流选取;探讨在自动构建河系树的基础上计算河流等级、所在层次等指标的方法;最后使用综合指标进行河流结构化选取试验。结果表明,以新等级规则为基础的综合指标切实可行,能够在一定程度上保持河网密度的区域差异。 相似文献
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98.
Sung-Soo Cha Kang-Kun Lee Gwang-Ok Bae Dae-Hyuck Lee Nicolas Gatelier 《Engineering Geology》2007,93(3-4):117-129
Hydrogeological monitoring was conducted around a pilot cavern for underground cryogenic LNG (Liquefied Natural Gas) storage. The monitoring was mainly focused on the operation of a drainage and recharge system. After the operation of the drainage system commenced, the drainage rate decreased rapidly in the initial stages and then decreased gradually. Hydrogeological monitoring revealed that the rock drainage system operated effectively. During drainage, the water table was maintained below the cavern roof. The recharge for ice-ring formation was performed in two phases. The first phase involved the cessation of pumping in downward-drainage holes and the second involved the closure of upward boreholes. Since the water table was maintained below the cavern roof, artificial recharge was planned at first. However, it was not implemented due to heavy rainfall in the recharge stage. On the basis of hydrogeological monitoring and hydraulic tests, it was found that the fractures above the roof and on the right wall of the pilot cavern mainly affected seepage into the cavern and thermal variation due to the storage of liquid nitrogen. Thermal variation was examined by the thermometers installed around the pilot cavern. The cooling and thawing processes reveal the characteristics of thermal distribution in the rock and the 0 °C isotherm. The cooling phase lasted for six months, and the 0 °C isotherm progressed in time after the injection of liquid nitrogen into the cavern. The isotherm propagated up to about 4 m from the floor and the sidewall of the cavern and about 3 m from the cavern roof. The cooling rate of the rock mass above the cavern roof was lower than that of the other cavern sides due to the gaseous space in the upper part of the containment. The fractures were analyzed and considered for thermal modeling. A two-dimensional finite element analysis was performed to compare the field monitoring at the pilot cavern. The numerical modeling shows the distance between the ice ring and heat transfer pattern of the fractures around the pilot cavern. The propagation of the measured and calculated 0 °C isotherm reveals that the water-conveying joint on the right wall might affect thermal propagation through a thermal pipe. 相似文献
99.
胡京红 《中国地质灾害与防治学报》2007,18(1):48-53
鲁山县四棵树河流域位于豫西伏牛山巨大的伏牛岩基东麓。区内山势陡峭,具大陆性季风气候,多暴雨,近期最大雨量116.9mm/h,日降雨达446mm。山洪泥石流是区内特有的一种自然地质灾害,它具有暴发频次高、暴发突然、流速快、破坏性大等特点,常冲毁道路、耕地和房舍,危及人民生命、财产安全。从对区内山地地形、气候、暴雨特征、岩性、土壤、泥石流及其造成的灾害状况等的调查、分析、研究,基本探索出泥石流运行轨迹即地表径流形成区、泥石流形成区、泥石流流通区、泥石流堆积区。根据上述特征,因地制宜地配置工程措施和非工程措施进行全面综合防治,重点对泥石流沟实施工程布防措施和山坡实施水土保持生物工程措施,对病险水库进行除险加固,从而达到标本兼治,防治泥石流灾害的发生和发展,改善生态环境,最终实现人与自然协调共处的目标。 相似文献
100.
Prediction of acid mine drainage generation potential in selected mines in the Ashanti Metallogenic Belt using static geochemical methods 总被引:1,自引:1,他引:1
Acid mine/rock drainage (AMD/ARD) is the biggest environmental threat facing the mining industry. This study investigates
AMD/ARD possibilities in three mines in the Ashanti Belt, using acid base accounting (ABA) and net acid generation pH (NAGpH)
tests. Twenty-eight samples of rock units and mine spoil from these mines were collected for ABA and NAGpH tests. Two tailing
dumps at Prestea and Nsuta were confirmed by both methods as acid generating with NAGpH of 4.5 and 4.6 and neutralization
potential ratio values of 4.38 and 4.60, respectively. Six other samples are classified as potentially acid generating using
a variety of established classification criteria. The rest of the samples either exhibited very low sulphur and carbonate
content or had excess carbonate over sulphur. Consistency between results from ABA and NAGpH tests validates these tests as
adequate tools for preliminary evaluation of AMD/ARD possibilities in any mining project in the Ashanti Belt. 相似文献