Movement characteristics of Karst water in a deep mining area

In order to study the movement characteristics of groundwater in a deep mining area and solve the dispute of the distri-bution rule of hydro-chemical zoning which is contradicted by lixiviation water zoning in a horizontal direction, we directed our attention to the source of deep groundwater, its seepage and hydro-chemical characteristics in a typical mining area. We used a neotectonic water-control theory, chemical and isotope methods, as well as a method for analyzing dynamic groundwater conditions. The results indicate that 1) Karst water in the deep and medium parts of this mining area is recharged by vertical leakage through neotectonic fractures rather than seepage along strata from subcrop parts or surrounding flows; 2) from surface to deep leakage paths, the variation in the types of chemical groundwater agrees with the normal lixiviation water distribution rule and the age of mixed groundwater increases; 3) the water-rich zones along neotectonic fractures correspond with water-diluted zones in a hori-zontal direction; 4) the leakage coefficient and water capacity of aquifers increases during the flow process of Kant water along the antidip direction (from west to east) and 5) Karst water in shallow mining areas forms a strong runoff belt along strikes and quickly dilutes the water from deep and medium mining areas. Overall, chemical and dynamic water characteristics actually agree with in terms of the entire consideration for differences in vertical leakage and abnormalities in the zone of water chemical distribution, along a horizontal runoff direction.     

Zonal disintegration phenomenon in enclosing rock mass surrounding deep tunnels -- Elasto-plastic analysis of stress field of enclosing rock mass

The zonal disintegration phenomenon (ZDP) is a typical phenomenon in deep block rock masses. In order to investigate the mechanism of ZDP, an improved non-linear Hock-Brown strength criterion and a bi-linear constitutive model of rock mass were used to analyze the elasto-plastic stress field of the enclosing rock mass around a deep round tunnel. The radius of the plastic region and stress of the enclosing rock mass were obtained by introducing dimensionless parameters of radial distance. The results show that tunneling in deep rock mass causes a maximum stress zone to appear in the vicinity of the boundary of the elastic and the plas-tic zone in the surrounding rock mass. Under the compression of a large tangential force and a small radial force, the rock mass in the maximum stress zone was in an approximate uniaxial loading state, which could lead to a split failure in the rock mass.     

关于抗冻胀设计规范中冻胀量预报的讨论

对渠系工程抗冻胀设计规范和水工建筑物抗冰冻设计规范中的冻胀量预报的理论,设计应用等问题进行了分析,针对存在的问题提出了计算（图表）方法、适用条件等改善建议。     

850农场地下水资源可持续开采利用研究

850农场是三江平原地下水开采强度最大农场之一,井灌面积占平原面积57.7%,现地下水埋深约5 m,处理想埋深中,地下水用量约405 m^3/hm^2·a,产量还略高于本场渠灌稻。本地区井灌面积达2.07×104hm^2,只要在节水灌溉上下功夫,可达采补平衡。若在雨洪资源化上下功夫,“西水东调”和建河滩“漏水库”,还可发展水田,水田比例由现0.577上升到0.60以上,故此850农场地下水可持续开采利用。     

“润发10”号子母海驳船组交付

仪征市润发船业有限公司为荷兰船东建造的“润发10”号子母海驳船组顺利交付。“润发10”号子母海驳船组由尺度不等的21艘出口驳船叠架组成。母驳船总长120米、型宽33米、型深7．6米、载重2万吨。船组叠架绑扎固定后．     

隧道埋深及开挖方法对于二衬支护时机的影响

为了研究隧道埋深和施工方法对二衬支护时机的影响,以广梧高速公路牛车顶隧道为工程背景,建立数值计算模型,分别改变隧道埋深和施工方法,得到相应的隧道二衬支护时机.结果表明：通过数值计算,可定量得到二衬及掌子面之间的允许距离和埋深的关系;当埋深较小时,二衬与掌子面的允许距离随着埋深的增加而增加;当埋深超过某一限值时,隧道二衬与掌子面的允许距离基本不变;开挖工法对二衬与掌子面间的允许距离影响比较显著,而对仰拱与掌子面的允许距离影响很小.随着开挖断面分部的增加,开挖对围岩的扰动减小,因而可以适当延缓构筑二衬时机.若选取Ⅲ级围岩中的全断面开挖法作为参考基准,则围岩中二衬与掌子面的允许距离将由于选择不同工法需进行修正,相应的修正值为：全断面法1.0,上下台阶法和中隔壁法均为1.5.     

全非线性深水波的Green-Naghdi理论研究

全非线性深水波的数值模拟对于深海工程有着重要意义.应用二维深水G-N理论的控制方程,得到深水LevelⅢ G-N理论和Level Ⅳ G-N理论的线性解析解.采用深水Level Ⅲ和Level Ⅳ G-N理论对单色波进行数值模拟.提出适用于G-N理论的非线性造波边界条件,使用线性造波边界条件的结果与使用非线性边界条件的结果基本一致,因此可以使用线性造波边界叠加的方法来模拟不规则波.采用深水LevelⅢG-N理论模拟全非线性双色波和不规则波,并与线性解析解进行比较,结果表明使用深水LevelⅢG-N理论并配合线性造波边界条件来模拟全非线性深水不规则波是可行的.     

医用局部深孔手术摄像照明装置

在五官科、脑外科手术中,由于光源的光轴与人眼睛的视轴无法完全重合,当手术部位距体表有一定深度时,人眼观察到的手术部位的某个边沿总有一部分区域存在阴影,孔越深两光轴夹角越大,阴影的区域越大。当某个细致部位需要仔细观察时,也无法放大．     

流沙易坍地层中超深钻孔桩施工技术总结

通过对流沙易坍地层中超深钻孔桩钻进的施工过程的论述,总结出此类地层中超深钻孔桩钻进施工的工艺方法和控制要点。     

不同引渠形式下深式短管进口泄流能力的试验研究

为研究红岩河水库导流泄洪洞深式短管进口引渠形式由明渠改成涵洞后对其泄洪能力的影响,对其在明渠和涵洞两种形式下分别做水工模型试验,验证其水力特性。结果表明,较明渠形式,涵洞形式下的导流泄洪洞同水位下泄流量有不同程度的减小,下泄流量减小在导流泄洪洞进口为压力流状态时表现明显,且减小值随水位的升高而变大;大坝度汛期100年一遇洪水时,试验下泄流量较设计下泄流量约小6.35%;运行期100年一遇洪水时,试验下泄流量较设计下泄流量约小6.51%;运行期2 000年一遇洪水时,试验下泄流量较设计下泄流量约小6.95%。建议在将红岩河水库导流泄洪洞深式短管进口引渠由明渠改成涵洞形式后,需关注导流泄洪洞的下泄流量减小问题,避免由于水库下泄流量不足引起的大坝安全问题。