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971.
972.
低丘红壤区不同降雨类型对浅层地下水位动态变化的影响——以江西省余江县为例 总被引:1,自引:0,他引:1
为研究低丘红壤区不同降雨类型对浅层地下水埋深的影响,在江西省余江县选择受自然因素影响较大的7口井进行分析。结果表明:影响浅层地下水水位变化的因素除了与降雨量、蒸发量、地表径流以及降雨过程中入渗土壤的雨水量外,还与降雨历时、降雨前期土壤的湿度等因素有关;据监测2 a的地下水位、降雨量等动态变化,从中选出三种降雨类型(Ⅰ降雨强度小且历时长,Ⅱ降雨强度大且历时短,Ⅲ干旱无雨时突然一场中雨),其中一场中雨就可以使Ⅰ的井水位剧烈变化,一场大雨可以使Ⅱ中的井水位明显抬升,偶尔一场大雨仅能湿润Ⅲ的土壤,对地下水位没有太多的影响;在浅层地下水位与降雨量、地表径流及进入土壤的雨水(RO)的相关性分析中,以降雨类型Ⅱ的相关系数的绝对值最大,且均呈极显著负相关,而降雨量与地表径流和RO呈极显著正相关。这表明在土壤周年盈水期且连续降雨时期,可对浅层地下水进行存储,以备在干旱少雨且作物需水时使用。 相似文献
973.
In the cold regions of northern China, incidents of municipal underground gas pipeline rupture and leakage occur quite frequently,
most often in winter. To prevent harm to citizen safety and property, analysis of the causes of such cracking and leakage is therefore
valuable. Two incident analyses are discussed here and the reasons why most of these types of cases occur during winter are clarified.
The effects of vehicle loadings above buried pipelines are calculated and compared with the effects and calculations of frost heaving
forces. We demonstrate that when the soil layer above a pipeline freezes rapidly, the soil generates repeated frost heaving, which exerts
heaving forces on the pipeline that can result in fatigue crack propagation and ultimate pipeline failure. Therefore, the incident induced
by frost heaving is one of the primary reasons of gas pipeline failure. Based on these analyses, we present some recommendations
pertaining to the proper design, construction, and management of gas pipelines. 相似文献
974.
经典天体测量仪器以铅垂线为基准测量本地的天文经纬度,因而能探测到本地铅垂线的偏转.本地铅垂线的偏转代表着测站周围重力场的变化,而这一变化与地下物质的再分布相关,由此有望帮助了解地下物质变化的情况.将本地的铅垂线偏转(Plumb Line Variation, PLV)与地下物质变化联系起来,建立了双质量体模型.在97°E–107°E和21°N–29°N范围内,考虑了3480个包含正、负质量变化(相对地质背景)的质量体组合算例,并利用差分进化(Differential Evolutionary, DE)算法进行了解算.解算得到的质量体相对于模拟值的位置误差小于米量级,质量误差小于1011kg,结果精度较高. 相似文献
975.
976.
977.
978.
通过对井下三角高程测量的原理、误差来源及精度分析,指出钢尺量取仪器高和棱镜高的误差对三角高程测量结果的影响,提出一种利用多元线性回归减小该误差影响的算法,并通过实例对三角高程测量结果进行改正,验证该算法用于提高井下三角高程测量精度是可行的,并基本达到四等水准的要求. 相似文献
979.
A. J. Cross D. J. Purdy D. C. Champion D. D. Brown C. Siégel R. A. Armstrong 《Australian Journal of Earth Sciences》2013,60(7-8):987-1008
AbstractZircon U–Pb ages, εHf(t), and δ18O isotopic data together with geochemistry and limited Sm–Nd results from magmatic rocks sampled in deep-basement drill cores from undercover parts of the Thomson Orogen provide strong temporal links with outcropping regions of the orogen and important clues to its evolution and relationship with the Lachlan Orogen. SHRIMP U–Pb zircon ages show that magmatism of Early Ordovician age is widespread across the central, undercover regions of the Thomson Orogen and occurred in a narrow time-window between 480 and 470?Ma. These rocks have evolved εHf(t)zrn (?12.18 to ?6.26) and εNd (?11.3 to ?7.1), and supracrustal δ18Ozrn (7.01–8.50‰), which is in stark contrast to Early Ordovician magmatic rocks in the Lachlan Orogen that are isotopically juvenile. Two samples have late Silurian ages (425–420?Ma), and four have Devonian ages (408–382?Ma). The late Silurian rocks have evolved εHf(t)zrn (?6.42 to ?4.62) and supracrustal δ18Ozrn (9.26–10.29‰) values, while the younger Devonian rocks show a shift toward more juvenile εHf(t)zrn, a trend that is also seen in rocks of this age in the Lachlan Orogen. Interestingly, two early Late Devonian samples have juvenile εHf(t)zrn (0.01–1.92) but supracrustal δ18Ozrn (7.45–8.77‰) indicating rapid recycling of juvenile material. Two distinct Hf–O isotopic mixing trends are observed for magmatic rocks of the Thomson Orogen. One trend appears to have incorporated a more evolved supracrustal component and is defined by samples from the northern two-thirds of the Thomson Orogen, while the other trend is generally less evolved and from samples in the southern third of the Thomson Orogen and matches the isotopic character of rocks from the Lachlan Orogen. The spatial association of the Early Ordovician magmatism with the more evolved metasedimentary signature suggests that at least the northern part of the Thomson Orogen is underlain by older pre-Delamerian metasedimentary rocks. 相似文献
980.