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1)  flow rate of well
钻孔涌水量
1.
To improve the flow rate of well is of importance to in-situ leaching of uranium in low permeable deposits.
提高钻孔涌水量是低渗透砂岩型铀矿床地浸开采的重要内容。
2)  water inrush borehole
涌水钻孔
1.
Discussion and study were made on drilling technology for water inrush borehole combined with the treatment of flush accident in zK0406 borehole of Pulang copper mining area in Shangrila.
结合香格里拉县普朗铜矿区ZK0406号钻孔涌水事故的处理,探讨和研究了涌水钻孔的钻进工艺,总结了施工经验和体会。
3)  gas emission during boring
钻孔瓦斯涌出量
1.
Based on analysis of the basic features of dynamic gas emission during boring, a phase space model for reconstruction of the dynamic characteristics by using the time series of gas emission from boring is put forward.
在此基础上,应用时序数据分析法,对实测得到的钻孔瓦斯涌出量序列进行计算分析,发现其具有分维特征。
4)  the drill hole returns the water method of variables
钻孔返水计量法
5)  drilling lost circulation water
钻孔漏失水量
6)  borehole dual piping experiment
双钻孔管涌试验
1.
Based on studying the matter component of faulted zone,the accurate and reliable calculating parameters were gotten through borehole dual piping experiment and parameter sensibility analysis,and the seepage gradients of fault zone and influence zone were calculated by analyzing different working condition in finite element methods.
在研究断层带物质组成的基础上,通过现场双钻孔管涌试验、参数敏感性分析取得了准确可靠的计算参数,并采用有限元数值法对不同工况进行分析计算求得了断层破碎带及影响带的允许渗透比降。
补充资料:饱和持水量测定


饱和持水量测定
measurement of saturation moisture capacity

  匕aohe ehishuiliang eeding饱和持水t测定(measurement of satu-ration moisture eaPaeity)土壤农业水文特性测定项目之一,是测定土壤孔隙完全充满水时的l几壤湿度。饱和持水t所占容积等于土壤总孔隙度,可用来鉴定土壤水分饱和程度和总孔隙度。 测定方法是浸水饱和法。即在欲测地段上,用容重环刀取原状土,取土方法与测定卜壤容重时取_L相同(见土壤容l测定)。把装有未遭破坏土样的环刀称重后,使其有孔底一端(内垫滤纸)朝下,放在盛水的平底磁盘中或充满水的砂层上,使盘内水面与环刀上缘保持一样高,切勿使水面淹没环刀,以免影响空气自土壤孔隙排出,使水不能充满孔隙。经过一定时间后(砂土4一8小时,粘土8一12小时)迅速取出,用盒盖托住称重。然后再放入盘中,继续使水充满孔隙,直至前后两次重量无显著差异为止。为了计算环刀中土体的干土重,必须在同一土层上,另取土样,用称重烘干法测其湿度。用下式计算饱和持水量(占干土重的百分数): 环刀中上样吸水饱和*、、、。_后的含水量吧刊’寸小里一环万币王释的不干甭入川U.式中上样干土重(克)=环刀中的湿土重(克)xl()0100十上样湿度的百分数 此外,通过下式也可计算饱和持水量(占干土重的百分数):饱和持水量二总孔隙度 容重火10()%式中总孔隙度二1一宣重比重(林家栋)
  
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