煤炭工程 ›› 2015, Vol. 47 ›› Issue (11): 39-41.doi: 10.11799/ce201511013

• 施工技术 • 上一篇    下一篇

白垩系软岩交圈前冻结壁扩展速度研究

李昆   

  1. 天地科技建井研究院
  • 收稿日期:2014-10-11 修回日期:2015-04-09 出版日期:2015-11-12 发布日期:2015-12-07
  • 通讯作者: 李昆 E-mail:414495497@qq.com

The expansion velocity research of cretaceous soft rock before the freeze wall circling

  • Received:2014-10-11 Revised:2015-04-09 Online:2015-11-12 Published:2015-12-07

摘要: 为研究白垩系软岩交圈前冻结壁扩展速度,以达到提前开挖的目的,运用回归分析的方法对白垩系软岩四个立井深水文孔冒水情况及去路盐水降温梯度进行研究得出:白垩系软岩地层设置浅层水文孔来预测冻结壁的交圈宜采用其他方法来代替;白垩系软岩交圈前冻结壁扩展速度V与去路盐水降温梯度T成线性关系,线性回归方程为V=-17.653T+12.444;白垩系软岩交圈前冻结壁扩展速度的经验值为25mm/d。

关键词: 白垩系软岩, 冻结壁, 回归分析, 扩展速度, 降温梯度

Abstract: For the study of freezing expansion speed of Cretaceous soft rock strata, in order to achieve the purpose of shaft excavation in advance. Through the study on the risk of four deep water hole and brine cooling gradient of soft rock strata in the Cretaceous, study concluded that: Asabu Minkong should be set carefully, and the prediction of shallow frozen wall to circle should use other methods to replace; the cretaceous soft rock freezing expansion rate of V presents the linear relationship with the way salt water cooling gradient T, linear regression equation V = -17.653T + 12.444;. And the research analysis puts experience value 25mm/d of the freezing expansion speed in soft rock strata of Cretaceous before ringing.

Key words: Cretaceous soft rock, frost wall, regression analysis, expansion speed, temperature gradient

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