Key Technique of Gas Sucking of "Three-Soft" Coal Bed and Its Application
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Research of anti-permeation mechanism of soft rock tunnel of shotcrete and its a nalogue experiment
In lingt of the anti-permeation performance problem of soft rock tunnel under the condition of shotcrete in glide structure area of West Henan,and from the basic theories of cube laws,combined with characteristics of laminar flow of ground water,and according to the different constructions condition,the analogue experiments of permeation properties of cementation plane are carried out;and homologous calculation formula are deduced.By comparison and analysis of the result,we can clearly understand the process and the mechanisms of interaction between various influence factors such as rock character,roughness,interface agent and large fluting,etc.It is concluded as follows:(1)as soft plane in constitution,permeation performance of cementation plane is far greater than that of rock mass and concrete;in the same,permeation performance of cementation plane of soft rock with coarse grain is also greater than that with fine grain;(2) restriction of roughness of rock mass,utilization of interface agent and set appropriate fluting on cementation plane can all increase its anti-permeation performance;and(3)load conditions of rock mass influence anti-permeation performance of cementation plane to a great extent.
Thorium-to-Uranium Ratios as Indicators of Sedimentary Processes: Example of Concept of Geochemical Facies
Because of analytical difficulties, few data are available on the thorium and uranium contents of sedimentary rocks. More than 200 new thorium and uranium determinations have been made by gamma-ray spectral technique and by an alpha activity-fluorometric uranium technique. Together these two independent techniques can be used as an experimental test of secular radioactive equilibrium. Only rarely in this study have fresh samples of ancient sedimentary rocks been found out of radioactive equilibrium. The accuracy of the thorium-to-uranium ratio determinations is more than sufficient for many geologic studies. The thorium-to-uranium ratios in sedimentary rocks range from less than 0.02 to more than 21. Ratios in many oxidized continental deposits are above 7, whereas most marine deposits have ratios much below 7. Thus, the thorium-to-uranium ratio varies with sedimentary processing and depositional environment. A cyclothem and several other sedimentary sequences illustrate the use of this ratio to distinguish environments and processes. The thorium content of shales varies much less than the uranium content. By mineral and trace-element analysis an attempt has been made to evaluate the resistate, hydrolyzate, clay, and precipitate (evaporite) contributions to the thorium and uranium contents of sedimentary rocks. These data also provide some insight into the details of the mobilization, tra sportation, and fixation of thorium and uranium in the sedimentary cycle. Field tests indicate that quantitative potassium, uranium, and thorium determinations can be made with a spectral gamma-ray logging instrument. Logs obtained with such instruments may provide an important additional means for subsurface interpretations.