饱和岩 meaning in English
saturated rocks
saturatedrock
Examples
- The travertine has the character of surviving and perishing together with karstic water , lacking of saturated karstic water , the travertine landscapes would be blacken , spalled , sanded , and collapsed
钙华具有“与水共存亡”之特性，失去饱和岩溶水滋养的钙华会变黑、剥落、砂化、垮塌。 - ( 2 ) on the basis of continuity equation , momentum conservation equation , energy conservation equation , and substantial equation , coupled thm governing equations are derivated with giving up the assumption of local thermal equilibrium , adopting thermal elasto - plastic constitutive relation , taking the effect of temperature gradient on groundwater seepage ( analogous to soret diffusion ) and the effect of viscous dissipation of groundwater on temperature field of rock mass into account
( 2 )根据连续性方程、线动量平衡方程和能量守恒方程以及相应的物性方程推导了饱和岩体温度场-渗流场-变形场三场耦合作用控制方程组。在推导控制方程组时舍弃了“局部热平衡”假设，采用了热弹塑性本构关系，考虑了温度梯度对地下水渗流的影响(类soret效应)以及地下水的粘性耗散对岩体温度场的影响。 - The following results were found , i . e . , the water ratio affects obviously the acoustic wave velocity of rock sample ; the wave velocity is higher in saturated rock samples than in unsaturated ones ; and it decreases gradually with the strain of samples during uniaxial compression ; and also with the lengthening holding time at 160 ; when heating the samples the acoustic wave velocity increases slightly in initial stage and comes to the peak value at 60 , then decreases gradually with increasing temperature ; meantime , there is a certain temperature effect on rock samples size
实验发现含水率对波速影响比较大，饱和岩样的声波传播速度高于不饱和岩样的声波传播速度；人工预制裂纹对声波传播速度影响不大；单轴压缩条件下，声波传播速度随应变增加逐渐降低；在同一温度( 160 )下，波速随保温时间的增加而逐渐降低；在对岩样逐渐加热情况下，初始加热阶段波速略有升高，当温度达到60时，岩样波速达到峰值，之后随着温度继续升高其波速逐渐下降；波速随温度变化具有一定的尺寸效应。 - After the saturated karstic spring was exposed to ground , for the changing of temperature , pressure , dynamics and the infecting of creatures , the ca / mgco3 deposited and turns into the travertine . the travertine heightened , and accumulated water to lakes , when the water brimmed over , waterfall came into being . this is the famous " stratified lakes and folded waterfalls " sight
该区钙华系饱和岩溶水出露地表后，因温度、压力、水动力条件发生改变，加上生物作用的影响， ca / mgco _ 3析出堆积而成，并逐渐加高潴水成湖；湖水充盈，叠水成瀑，从而形成了沿沟谷底层层叠叠分布的“层湖叠瀑”奇景组合。