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深井底板突水模式及其突变特征分析

尹立明 郭惟嘉 路畅

采矿与安全工程学报2017,Vol.34Issue(3):459-463,5.
采矿与安全工程学报2017,Vol.34Issue(3):459-463,5.DOI:10.13545/j.cnki.jmse.2017.03.09

深井底板突水模式及其突变特征分析

Patterns of the water-inrush hazard in the floor strata in deep mines and its catastrophic characteristics

尹立明 1郭惟嘉 1路畅1

作者信息

  • 1. 山东科技大学矿山灾害预防控制国家重点实验室(培育),山东青岛266590
  • 折叠

摘要

Abstract

With the formation mechanism of conductor on floor water-inrush as the division criterion,the floor water-inrush patterns in deep mining was divided into three categories:the whole aquifuge type,the buried structure type,and the intrinsic conductor type.The introduction of cusp catastrophe model into the whole aquifuge type and the intrinsic conductor type built the butterfly catastrophe model which was applied to the buried structure type.The catastrophic characteristics of floor water-inrush hazard in deep mines were analyzed based on the geometric properties of the equilibrium surface of the cusp catastrophe model.This study has shown that 1).From time perspective the water-inrush hazard of floor strata in deep mines has the character of burstiness and lagging;2).From space perspective,catastrophe paths of the hazard in the floor strata have the character of diversity,and the water-inrush location in the buried structure type and the intrinsic conductor type has its regularity.

关键词

深部开采/底板突水灾害/突水模式/突变特征

Key words

deep mining/water-inrush hazard of floor strata/evolution mode/catastrophic character

分类

矿业与冶金

引用本文复制引用

尹立明,郭惟嘉,路畅..深井底板突水模式及其突变特征分析[J].采矿与安全工程学报,2017,34(3):459-463,5.

基金项目

国家自然科学基金项目(51404144,U1361105) (51404144,U1361105)

中国博士后科学基金项目(2015T80731,2014M551936) (2015T80731,2014M551936)

山东省博士后创新项目(201302018) (201302018)

采矿与安全工程学报

OA北大核心CSCDCSTPCD

1673-3363

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