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51.
The Geothermal Study of the Mid-Segment of the Tancheng-Lujiang Fault Zone and Its Neighboring Region 总被引:1,自引:0,他引:1
In this paper,25 new terrestrial heat flow values newly observed along the mid-segment of the Tancheng-Lujiang fault zone are listed.With these geothermal data and 37 other terrestrial heat flow values(previously published),we describe the distribution features of terrestrial heat flows in the area.In this research,the two-dimensional temperature structure from the surface to lithospheric bottom of the Huaibei-Sixian-Jinhu profile is inferred by using the finite-element method and the temperature and heat flow of sedimentary,granitic,and basaltic layers is calculated. 相似文献
52.
Heterogeneous characteristics of streambed saturated hydraulic conductivity of the Touchet River,south eastern Washington,USA 总被引:1,自引:0,他引:1
Randal Leek Joan Q. Wu Li Wang Timothy P. Hanrahan Michael E. Barber Hanxue Qiu 《水文研究》2009,23(8):1236-1246
Traditionally a streambed is treated as a layer of uniform thickness and low saturated hydraulic conductivity (K) in surface‐ and ground‐water studies. Recent findings have shown a high level of spatial heterogeneity within a streambed and such heterogeneity directly affects surface‐ and ground‐water exchange and can have ecological implications for biogeochemical transformations, nutrient cycling, organic matter decomposition, and reproduction of gravel spawning fish. In this study a detailed field investigation of K was conducted in two selected sites in Touchet River, a typical salmon spawning stream in arid south eastern Washington, USA. In‐stream slug tests were conducted to determine K following the Bouwer and Rice method. For the upper and lower sites, each 50 m long and 9 m wide and roughly 20 m apart, a sampling grid of 5 m longitudinally and 3 m transversely was used. The slug tests were performed for each horizontal coordinate at 0·3–0·45, 0·6–0·75, 0·9–1·05 and 1·2–1·35 m depth intervals unless a shallower impenetrable obstruction was encountered. Additionally, water levels were measured to obtain vertical hydraulic gradient (VHG) between each two adjacent depth intervals. Results indicated that K ranged over three orders of magnitude at both the upper and lower sites and differed between the two sites. At the upper site, K did not differ significantly among different depth intervals based on nonparametric statistical tests for mean, median, and empirical cumulative distribution, but the spatial pattern of K varied among different depth intervals. At the lower site, K for the 0·3–0·45 m depth interval differed statistically from those at other depth intervals, and no similar spatial pattern was found among different depth intervals. Zones of upward and downward water flow based on VHG also varied among different depth intervals, reflecting the complexities of the water flow regime. Detailed characterization of the streambed as attempted in this study should be helpful in providing information on spatial variations of streambed hydraulic properties as well as surface‐ and ground‐water interaction. Copyright © 2009 John Wiley & Sons, Ltd. 相似文献
54.
已发表的三个脉冲星星表共有384颗。采用这个样本并用一种经验的方法修正观测选择效应,获得脉冲星按银心距离的分布和银河系中可能存在的脉冲星总数。一个明显的峰值在离银心5—7KPC处。脉冲星的总数为(8.4±3.7)×10~4。采用束因子值为5和平均寿命为9×10~6年,得到诞生率为每15—38年产生一颗。 相似文献
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57.
腰椎管侧隐窝分型及影响侧隐窝狭窄症诊断的几个因素(附120例CTM分析) 总被引:1,自引:0,他引:1
作者对120例因下腰痛手术治疗在术前进行过CTM检查的患者作了影像学及临床分析.按形态不同,侧隐窝可分为五种类型:(1)三角型,即整个椎管呈倒三角形,其侧隐窝完全开放;(2)猫耳型,因后关节和椎体后缘轻度增生,形成底宽顶尖的侧隐窝,整个椎管形如猫头,侧脸窝为猫耳,基本开放;(3)牛角型,因关节突向椎体方向过度增生使侧隐窝呈横向伸开的带状,中央椎管不窄,横断面形如牛头,侧阴窝为牛角,严重者侧隐窝可近于闭塞;(4)三叶草型,极度增生的关节突加上向后实入的椎体后缘使整个椎管呈三叶草状,侧隐窝和中央椎管均狭窄;(5)混合型,多为上述形状的混合或两侧侧隐窝发育不对称.前二型不易形成对神经的压迫,后三型易造成压迫.但即使最狭窄的侧隐窝也不一定产生症状,因为关键在于神经根和侧隐窝的宽度的相对关系.因此作者提出单纯依靠侧隐窝的宽度不能诊断侧隐窝狭窄症,而是要判断神经是否被侧隐窝压迫.因此CTM在侧隐窝狭窄症的诊断中有突出意义. 相似文献
58.
本文分析了威海市杨家滩不源地第四系冲洪积-海相沉积物分规律和水文地质特征;在此基础上,应用有限单元方法进行了地下水量评价和预测水源地地下水位的变化趋势;提出了最优开采方案。 相似文献
59.
Study of Influence of Regional Geodynamic Background on Strata Behaviors in China's Tongxin Mine 下载免费PDF全文
Strata behaviors are mainly affected by regional geodynamic background. The influence of rock mass stress and energy distribution on strata behaviors in the Tongxin mine is studied in terms of regional tectonic movement, seismic activity and tectonic stress field. The results show that the extrusion lifting movement of Kouquan fault adjacent to the Tongxin mine results in the stress concentration in the rock of the Carboniferous coal bed and accumulation of a large amount of elastic energy and forms structural background of Tongxin mine. Due to various seismic activities in the mine area, the strain energy is known to reach much higher levels, up to 0.5×108 J1/2. Since the stratigraphic structure is sensitive to the mining operation, the strain energy could cause strong strata behaviors. A special geological structure model of the Tongxin mine is established based on the geodynamic division method. The distribution of regional structure stress field is determined by the rock mass stress analysis system. Based on this model, Tongxin mine is divided into five areas with high stress, eight areas with low stress and eight areas with gradient stress. The strong strata behaviors mostly occur in high stress areas. These results could provide guidance to predict the strength of regional or mine pressure and control strata behavior in different areas. 相似文献
60.