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991.
对北京地区超采引起的地下水位动态特征与成因作了详细分析,并对超采背景下如何提取地震前兆异常信息的问题作了探讨.北京地区地下水位年动态的主要影响因素是地下水开采和降雨,而地下水位动态的趋势变化则与区域地下水超采量有直接关系.本文用相关分析的方法,分析了北京平原区超采量与水位变化之间的关系,为评价超采区观测井的干扰影响程度、识别地震前兆信息提供依据.研究结果表明,在区域超采不严重的地区引起的水位趋势性变化中,也包含着地震前兆信息;采用消除趋势及年变化影响的数学处理方法,可提取出地震的趋势异常变化. 相似文献
992.
993.
994.
页岩孔隙研究新进展 总被引:9,自引:0,他引:9
随着非常规油气勘探的兴起页岩孔隙研究备受重视,如何研究页岩孔隙已经成为非常规油气首要解决的问题之一,其对页岩油气勘探层位选取、资源潜力评价和油气渗流能力计算具有重要意义。对页岩微—纳米孔隙表征技术、页岩孔隙类别的划分以及页岩孔隙演化规律分别进行了综述并指出存在问题,同时结合最新研究进展对页岩孔隙研究进行展望。提出工业CT—微米CT—纳米CT/FIB系列辐射扫描方法和压汞(MICP)—氮气吸附(N2)—二氧化碳吸附(CO2)流体法是孔隙定量表征的最优方法,通过单井孔隙度测井资料与实验室测定结果建立校正图版指导储层孔隙发育段优选;页岩孔隙分类研究还应该考虑含油气性,利用原子力显微镜等工具加强孔隙含油性研究;孔隙演化规律研究应该采用模拟实验和真实剖面样品对比并结合矿物组成分析等寻找主控因素。 相似文献
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996.
利用多目标区域地球化学调查高精度和高密度土壤碳分布数据,建立单位土壤碳量,采用指数模型计算方法,取得各地区土壤碳储量数据.按照土壤类型、土地利用分类、生态系统及自然景观等划分方式,按照 0~0.2m,0~1.0m和 0~1.8m不同土壤深度,分析了四川、湖南、吉林、江苏、河北、陕西等代表性地区有机碳储量空间分布特征,进行中国土壤碳储量研究.计算结果表明,全国土壤碳储量分布不均匀.按照 0~1.8m深度比较,成都平原土壤碳储量为1462.9Mt,碳密度为24813t/km2; 吉林平原区碳储量1381.96Mt,碳密度14473t/km2; 湖南洞庭湖区碳储量757.65Mt,碳密度18171t/km2; 江苏省碳储量1468.87Mt,碳密度13802t/km2; 陕西渭河平原碳储量165.47Mt,碳密度12124t/km2; 河北平原区碳储量844.84Mt,碳密度10525t/km2.按照面积加权平均计算,推算出全国多目标区域地球化学调查地区平均碳密度,0~0.2m为3186t/km2,0~1.0m为11646t/km2,0~1.8m为15339t/km2. 相似文献
997.
998.
Up to now, exact measurements of chromospheric magnetic fields have not been as successful as those done in the photosphere. We are currently engaging in diagnostics of chromospheric magnetic fields with the Mg b2 line by employing the Multi-Channel Solar Telescope at Huairou Solar Observing Station. Therefore, how to improve accuracy in the measurement is the main issue of our present study. To this end, we first study linear calibration coefficients for longitudinal and transverse components of chromospheric fields, which vary with wavelength, in the case of a weak field assumption. Then the polarization crosstalk introduced by instruments is analyzed in detail with two numerical simulation methods. Comparisons of the po- larization signals between cases with and without correction are presented. The result indicates that polarization accuracy is greatly improved after crosstalk correction. 相似文献
999.
Crustal structure of the Paleozoic Kunlun orogeny from an active-source seismic profile between Moba and Guide in East Tibet, China 总被引:13,自引:0,他引:13
Zhongjie Zhang Simon Klemperer Zhiming Bai Yun Chen Jiwen Teng 《Gondwana Research》2011,19(4):994-1007
We herein present a new seismic refraction/wide-angle reflection profile that crosses the Songpan–Ganzi terrane, the Animaqing suture zone and the eastern Kunlun mountains (comprised of the South Kunlun and Middle Kunlun blocks separated by the Middle Kunlun fault). The profile is 380 km long and extends from Moba to Guide in eastern Tibet. The crustal thickness is about 62 km under the Songpan–Ganzi terrane, 62–64 km under the South Kunlun, and 60 km under the Middle Kunlun block. The Songpan–Ganzi flysch seems to be present up to a depth of 15 km south of the Animaqing suture zone, and up to a depth of 10 km in the Middle Kunlun block, with thicknesses elsewhere that depend on assumptions about the likely lithologies. The profile exhibits clear lateral variations both in the upper and lower crust, which are indicative of different crustal blocks juxtaposed by the Kunlun fault system. Whether or not the Songpan–Ganzi flysch was originally deposited on oceanic crust, at the longitude of our profile (100°E) it is now underlain by continental crust, and the presence of continental crust beneath the Songpan–Ganzi terrane and of a continental arc under the South Kunlun block suggest Paleozoic continent–continent arc collision in the eastern Kunlun Mountains. Comparison of crustal velocity columns from all wide-angle seismic profiles across the eastern Kunlun mountains indicates a remarkable west-to-east change in the Moho topography across the Kunlun fault system (15–20 km Moho step at 95°E, but only 2–5 km along our profile at 100°E). Lower-crustal thickness of the Kunlun terranes is rather uniform, about 35 km, from 80°–95°E, which suggests that similar thrust-thickening processes have played a role where the Qaidam Basin abuts the Kunlun fault, but thins to 20–25 km at 100°E, east of the Qaidam Basin. The increased crustal thickness from 93° to 98°E compared to that at 100°E may be due to the differences in the thickness of the crust of the two plates before their collision, and/or largely achieved by thickening of the lower crust, perhaps indicating a crustal flow mechanism operating more strongly in the western region. 相似文献
1000.
GIS-based rare events logistic regression for landslide-susceptibility mapping of Lianyungang,China 总被引:6,自引:2,他引:4
Shibiao Bai Guonian Lü Jian Wang Pinggen Zhou Liang Ding 《Environmental Earth Sciences》2011,62(1):139-149
Landslides have had a huge effect on human life, the environment and local economic development, and therefore they need to
be well understood. In this study, we presented an approach for the analysis and modeling of landslide data using rare events
logistic regression and applied the approach to an area in Lianyungang, China. Digital orthophotomaps, digital elevation models
of the region, geological maps and different GIS layers including settlement, road net and rivers were collected and applied
in the analysis. Landslides were identified by monoscopic manual interpretation and validated during the field investigation.
To validate the quality of mapping, the data from the study area were divided into a training set and validation set. The
result map showed that 4.26% of the study area was identified as having very high susceptibility to landslides, whereas the
others were classified as having very low susceptibility (47.2%), low susceptibility (22.21%), medium susceptibility (14.39%)
and high susceptibility (11.93%). The quality of the landslide-susceptibility map produced in this paper was validated, and
it can be used for planning protective and mitigation measures. The landslide-susceptibility map is a fundamental part of
the Lianyungang city landslide risk assessment. 相似文献