龙王庙北矿水文地质特征及地下水流场模拟
DOI:
作者:
作者单位:

作者简介:

通讯作者:

基金项目:

宿州学院科研平台开放课题:宿县矿区地下水流场模拟及矿井水资源化评价(2015ykf12)


Hydrogeological Characteristics and Simulation of Groundwater Flow Field in Longwangmiao North Mine
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
    摘要:

    以龙王庙北矿地下水为研究对象,通过整理矿区基础资料,分析得出该矿水文地质特征。利用GMS软件建立地下水流 场模型,模拟结果为:区内地下水水位北高南低,东南部水位最低。地下水主要由矿区北部流向东南部;北部接收降雨补给,并 渗流至深处,浅层的垂向流速比深层的垂向流速大,北部深层地下水向南部的浅层径流,进而蒸发排泄。模拟结果与实际地下 水径流特点基本一致,则此次模拟参数设置合理,模拟结果较为可靠。

    Abstract:

    The north of groundwater of the Longwangmiao mine was studied as the research object. The hydrogeological characteristics of the mine are analyzed by sorting out the basic data of the mining area. The groundwater flow field model has been established by using GMS software. The simulation results show that the groundwater level is high in the north and low in the south, while the water level in the southeast is lowest. The groundwater mainly flows from the northern part of the mining area to the Southeast. The north receives rainfall supplies and seeps into the depths, and the vertical velocity of shallow layer is larger than that of deep layer. The deep groundwater in north run off to the south of mine, and then evaporated. The simulation results are basically consistent with the actual groundwater runoff characteristics. So the simulation parameters are reasonable and reliable

    参考文献
    相似文献
    引证文献
引用本文

郭 艳,曹志颖.龙王庙北矿水文地质特征及地下水流场模拟[J].西昌学院学报(自然科学版),2018,(1):38-41.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
历史
  • 收稿日期:
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期: 2018-04-21