Geological and Hydrogeological Framework of the Basin

求翻译，很急，帮帮忙~

1.1.1 origin project
Daerhanq is a border based on animal husbandry in Inner Mongolia pastoral flag, its economic, political and cultural centre of bailingmiaozhen is now located in the basin of the AI does not cover water supply source of sheep along the field, the existing water supply capacity of 5000m3/d. On the basis of baotou Daerhanq urban development planning, future Daerhanq and baotou baiyunebo area merged in Bayan OBO, bailingmiaozhen as its seat of municipal government. Urban residents in 2020 will reach 70,000 people need 15000 m3/d of water.
To address the bailingmiaozhen planning, drinking water, original geological prospecting in Inner Mongolia project tender organization of experts of the Commission on "Daerhanq bailingmiaozhen water supply hydrologic geology of Inner Mongolia detail" project was proof, that within the scope of 655km2 near the Daerhanq uher Hudag basin are expected to be completed daily supply possibility of 10000 m3 of water. Accordingly, the original Office of geological detail in Inner Mongolia project bidding Committee on July 2, 2008, 1-7 2008-water prospecting issued "geological exploration projects in geological prospecting in Inner Mongolia project bidding Committee assignments", borne by our "Inner Mongolia Daerhanq bailingmiaozhen water supply hydrologic geological detail".
1.1.2 objectives
The overall objective of the project is a basic hydrogeological conditions in identifying work areas, looking for 10000 for Daerhanq bailingmiaozhen of M3/d water, preliminary evaluation of groundwater resources, groundwater allowable withdrawal reach c-level accuracy requirements, to provide a basis for preliminary design of water source. Its specific tasks are:
1, the full collection, analysis and research work of meteorological, hydrological, geological, hydrogeological and other relevant information.
2, basic identifying basin geological structure of the tertiary aquifer conditions and spatial distribution and variation of water quantity, water quality.
3, basic identifying work fill diameter drainage conditions of groundwater in the region.
4, through the hydro-geological mapping, drilling, testing, and other means to determine the rich water section, select water supply sources, calculation and evaluation of groundwater resources

Wild river county for shenmu grotto major rivers of the Yellow River level, originating in DongShengShi tributary baal within the territory of the PRC shall DongShengShi, YiJinHuoLuoQi through ditch, the shenmu county, shaanxi province GeTai inflows aliena stone territory were ulam wood Aaron river, said in the store with NiuChuan intersection circumbendibus tower after the wild river, span called grotto 228km, a basin of 8706km2, XianJing 159km, XianJing keep basin of include large willow tower, chicken, jia bifurcation, hemp home tower, shop tower, shenmu town, baluster fort, solution home fort, tai village, sand Mao, HeGuChuan 11 towns, plan of the 3578km2, 46.86% of the total area. The main ZhiGou divan wild river WuSu ditch, often have test home ditch, hemp home tower ditch, XiGou, leiyang ditch, etc. So the wild river basin of grotto water environmental carrying capacity of research has important economic significance and social significance.

This paper based on the predecessor of the survey data and the wild river area grotto hydrological, geological and hydrogeological conditions, the paper analyzes the research of water environment pollution environment, including the analysis and water quality analysis, etc. On the basis of single factor pollution index method using water environment of research made evaluation, the results showed that the grotto wild river water in addition to the individual, the excess individual items with the other living standards for drinking water, for good or better living and drinking water. Zone for good or better groundwater life drinking water. Industrial water charges for good general boiler water samples, but for the average individual poor boiler water.

Wild river pollution PingShuiQi divan with relatively serious, main pollutants as petroleum, volatile phenol, ammonia nitrogen etc, mine drainage and coal related industrial waste water discharge of surface water environment pollution is serious, and with the rapid development of regional economy into the water quality deterioration.

Meanwhile integrating with environmental status and the calculation and analysis of the wild river basin of grotto forward prevention and control of water environment and measures.

As an intracratonic sedimentary basin，the Sichuan Basin occupies 200000 km2in southw estern China. The Basin contains 5 － 11 km of sediments w hich range in age from Sinian to Cretaceous. From the Late Sinian to the M iddle Triassic the basin w as under a marine condition. Limestone is the main rock of Ordovician， Devonian and Permian System ，and formations of Late Sinian，Cambrian，Carboniferous，and Low er and M iddle Triassic are cyclic carbonate-evaporite sediments. Only the Permian and the Low er and M iddle Triassic formations are continuous across the basin. The Upper Triassic formations that follow are interbedded sandstone and shale， w hich deposited in continental environments. The overlying Jurassic and Cretaceous system are red beds of mudstone w ith interbeds of sandstone. There are more than 300 anticlines in the basin ( Figure 19. 2 ) . Anticlines in the eastern-southeastern basin are long ，narrow ones，w hereas sedimentary strata are almost horizontal in the central-w estern basin. M ore than 20 brine-bearing aquifers of different age，w hich consist mainly of limestone and sandstone，have been identified. M ost of the brine-bearing aquifers occur w ithin Triassic rocks. Brines accompanied by natural gas as w ell as oil are often found rich in a number of anticlines. Hydraulic connection among aquifers and lateral flow of the brines in an aquifer are thought to be insignificant. Summaries of general lithology ，thickness for the aquifers and structure， hydrogeologic element of the basin can be found in Zhou and Li ( 1992 ) .

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