Numerical Simulation and Prediction of Mine Water A Case Study in Dangtu County of Anhui Province.docVIP
- 1、本文档共6页,可阅读全部内容。
- 2、有哪些信誉好的足球投注网站(book118)网站文档一经付费(服务费),不意味着购买了该文档的版权,仅供个人/单位学习、研究之用,不得用于商业用途,未经授权,严禁复制、发行、汇编、翻译或者网络传播等,侵权必究。
- 3、本站所有内容均由合作方或网友上传,本站不对文档的完整性、权威性及其观点立场正确性做任何保证或承诺!文档内容仅供研究参考,付费前请自行鉴别。如您付费,意味着您自己接受本站规则且自行承担风险,本站不退款、不进行额外附加服务;查看《如何避免下载的几个坑》。如果您已付费下载过本站文档,您可以点击 这里二次下载。
- 4、如文档侵犯商业秘密、侵犯著作权、侵犯人身权等,请点击“版权申诉”(推荐),也可以打举报电话:400-050-0827(电话支持时间:9:00-18:30)。
- 5、该文档为VIP文档,如果想要下载,成为VIP会员后,下载免费。
- 6、成为VIP后,下载本文档将扣除1次下载权益。下载后,不支持退款、换文档。如有疑问请联系我们。
- 7、成为VIP后,您将拥有八大权益,权益包括:VIP文档下载权益、阅读免打扰、文档格式转换、高级专利检索、专属身份标志、高级客服、多端互通、版权登记。
- 8、VIP文档为合作方或网友上传,每下载1次, 网站将根据用户上传文档的质量评分、类型等,对文档贡献者给予高额补贴、流量扶持。如果你也想贡献VIP文档。上传文档
查看更多
Numerical Simulation and Prediction of Mine Water A Case Study in Dangtu County of Anhui Province.doc
Numerical Simulation and Prediction of Mine Water A Case Study in Dangtu County of Anhui Province
【Abstract】In this paper, the regional groundwater flow system in Zhong Jiu iron ore was generalized into three-dimensional unsteady groundwater flow systems with homogeneous, isotropic and no boundary limits. The software of Visual MODFLOW was used to simulate and predict the gushing process. the conclusion was that the calibrated parameters were reasonable and the predicted value can satisfy the demand of the consumption of mining.
【Keywords】 Zhong Jiu iron ore, Hydrogeological conditions, Visual MODFLOW, Numerical simulation, Water inflow predicting.
Numerical method includes four steps: hydrogeological model conceptualization, building mathematical model, model calibration, mine water inflow predicting ect.
1 The Establishment of the Hydrogeological Conceptual Model
The mine area was in water-bearing medium that has no obvious water boundary, there are many clear differences among different water-bearing rock groups or even the same ones, but there are still some hydraulic connections. So, the anisotropy aquifer medium that above -370 meters in mining area was identified as the flow field , which is isotropic and has no confined boundary.
In order to reflect the geologic feature,the aquifers were generalized into 10 layers. The simulated range was 143km2 around the mine. The boundary was generalized as general head boundary and the simulation area was regarded as heterogeneous isotropic. The ground water flow was defined as transient flow that obey the Darcys law.
2 The Determination of Initial Conditions
The initial flow field was drawn based on the date of the water level in december 2009, The ten aquifer groups had different initial flow fields because of the minor differences among them and the minor groundwater exploitation quantities.
3 Mathematical Model of Groundwater Flow
3.1 Discretization
In space, according to geologic
文档评论(0)