[资料原创]Chemical grouting and soil stabilization 2003 PDF [复制链接]

Chemical grouting and soil stabilization 2003  e~t}z_>F  
|7S4;  
共22章  6个附录 内容很全面，共同学习 =& Tu`m  
contents I9*BENkR  
Chap 1-10

Chemical grouting and soil stabilization 2003  e&H<lT  
MOqA$b  
共22章  6个附录 内容很全面，共同学习 M|Dwk3#  
contents 3'sWlhf;  
Chap 11-22 /K1$_  
App

Under the action of gravity, surface water and groundwater always tend to
_[OEE<(  
flow from higher to lower elevations. Surface water will flow over solid and VrGb;L'[  
through permeable formations, and its volume and velocity are a function of FUqhSW  
the available supply and the fluid head. Groundwater can move only rd
35)  
through a pervious material (fractured or fissured rock or soils with G|G?h  
interconnected open voids), so its flow characteristic is also a function of c7nk~K[6  
formation permeability. Groundwater elevation varies as the supply source E=1/  
varies and can be raised or lowered locally by increasing or decreasing the l#vw L15  
local supply (naturally by precipitation or artificially by pumping a well or u.L8tR:(  
irrigating). In general, over a large surface area, groundwater surface is a a@=36gx)  
subdued replica of ground surface.

                         

收藏了，好贴！

谢谢楼主。这资料对我帮助很大！