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871.
口泉沟南水源地环境同位素研究和水资源评价 总被引:3,自引:0,他引:3
分析了大同矿区口泉沟南区的水文地质条件,利用氢,氧,铀,硫,碳等环境同位素研究了口泉南与相邻的泉域和三层洞泉域的关系及地下水的补给来源;用有限元法进行了地下水资源评价和水位预报,证明在该区建立供水10^4m^3的水源地是可能的。 相似文献
872.
应用直流电法仪在井下进行了工作面巷道底板电测深和掘进头超前探测,查清了工作面底板水层的富水性和掘进头前头的地质构造及含水情况。目前,大部分探测结果已得到生产实践的证实。 相似文献
873.
甘肃桦树沟(铁)铜矿床的成因机制 总被引:4,自引:0,他引:4
矿床地质地球化学特征研究结果表明,随着古陆边缘弧-槽-盆体系的发生与发展,元古代基底火山(沉积)岩系经深循环水(海水)-热系统的作用,成矿物质被浸出和搬运,并经海底喷溢作用沉淀于海盆洼地中形成桦树沟矿床含铜建造,后期变质作用使成矿物质活化、转移和富集。桦树沟矿床为喷气(流)沉积-变质改造型(铁)铜矿床。 相似文献
874.
Todor Ganev Fumio Yamazaki Tsuneo Katayama Teruyuki Ueshima 《Soil Dynamics and Earthquake Engineering》1997,16(7-8):459-470
This paper presents results from forced vibration tests, microtremor observations and earthquake response analysis of a nuclear reactor containment model constructed on stiff soil in Hualien, Taiwan. The dynamic behavior of the soil-structure system is simulated successfully with two numerical models: a sway-rocking model, whose soil parameters are evaluated on the basis of the continuum formulation method, and a finite element model, using the program SASSI with the flexible volume substructuring approach. The dependences of the soil parameters of both models on the amplitudes of the different dynamic excitations are investigated in detail. An original numerical simulation of microtremor is performed. Comparison with results of a previous study involving a rigid tower on a soft soil site in Chiba, Japan is offered. 相似文献
875.
The identifiability of parameters in a water quality model of the Biebrza River, Poland 总被引:1,自引:0,他引:1
The identifiability of model parameters of a steady state water quality model of the Biebrza River and the resulting variation in model results was examined by applying the Monte Carlo method which combines calibration, identifiability analysis, uncertainty analysis, and sensitivity analysis. The water quality model simulates the steady state concentration profiles of chloride, phosphate, ammonium, and nitrate as a function of distance along a river. The water quality model with the best combination of parameter values simulates the observed concentrations very well. However, the range of possible modelled concentrations obtained for other more or less equally eligible combinations of parameter values is rather wide. This range in model outcomes reflects possible errors in the model parameters. Discrepancies between the range in model outcomes and the validation data set are only caused by errors in model structure, or (measurement) errors in boundary conditions or input variables. In this sense the validation procedure is a test of model capability, where the effects of calibration errors are filtered out. It is concluded that, despite some slight deviations between model outcome and observations, the model is successful in simulating the spatial pattern of nutrient concentrations in the Biebrza River. 相似文献
876.
Crustal structure of Dabieshan orogenic belt 总被引:2,自引:0,他引:2
Chunyong Wang Xiankang Zhang Buyun Chen Xuebo Chen Songyan Song Jinhan Zheng Hongxiang Hu Hai Lou 《中国科学D辑(英文版)》1997,40(5):456-462
The crustal structures ofP velocity and density on the deep seismic sounding profile across the Ilabieshan orogenic belt are presented. There is a 5-km-thick
crustal “root” between the Yuexi and Xiaotian where the elevation is highest on the profile. An apparent Moho offset of 4.
5 km beneath the Xiaotian-Mozitan fault marks the paleo-suture of the Triassic collision. A high-velocity anomaly zone at
the depth below 3 km beneath the ultra-high pressure (UHP) zone may be correlated to the higher content of UHP metamorphic
rocks.
Project supported by the National Natural Science Foundation of China and the Joint Earthquake Science Foundation. 相似文献
877.
Numerical modeling of 3-D terrain effect on MT field 总被引:1,自引:0,他引:1
Using the boundary element method, the numerical modeling problem of three-dimensional terrain effect on magnetotelluric (MT)
field is solved. This modeling technique can be run on PC in the case of adopting special net division. The result of modeling
test for 2-D terrain by this modeling technique is basically coincident with that by 2-D modeling technique, but there is
a great difference between the results of 3-D and 2-D modeling for 3-D terrain.
Project supported by the National Natural Science Foundation of China. 相似文献
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