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1.
对辽宁金州地震台地下水位上升引起水准基岩标石底部岩层的应力变化进行定性和定量分析,并使用分层总和法计算基岩标石受到的影响量.研究结果表明,金州水准所受地下水的干扰,主要是标石底部的基岩在地下水位变化的作用下而发生形变所致,其影响的大小与水位变化幅度、水容重、基岩的压缩模量和孔隙度有关.  相似文献   

2.
采用主成分分析方法研究降水对地下水位的影响   总被引:2,自引:0,他引:2  
郑小菁  刘序俨  韦永祥  陈莹 《地震》2008,28(4):91-102
基岩裂隙地下水的井水位变化是一个受综合因素影响的观测量。 文中采用主成分分析方法, 分析了福建晋江青阳基岩裂隙水观测井2007年3~8月的地下水位观测资料, 并分别与降水当天值和降水累加值进行了对比研究, 讨论了两种计算结果。 根据计算结果分析认为, 基岩裂隙水观测井的地下水位对当天降水值的响应不显著, 主成分分析中的第一综合量主要为水位本身的得分, 而第二种情况得到的结果则分别反映了3~8月份逐月降水累加值对水位的影响, 说明降水对水位的影响具有累加效应, 并对5~8月份造成这种累加效应不明显的情况进行了探讨, 给出了逐月水位与降水累加值的逐月第一与第二综合量曲线。  相似文献   

3.
隐伏走滑断层破裂扩展特征的实验研究   总被引:4,自引:2,他引:4       下载免费PDF全文
通过模拟实验研究了基岩中走滑断层在上覆沉积层中的破裂扩展特征,利用白光数字散斑相关方法分析了沉积层表面变形场的演化过程,重点研究了基岩断层位移和沉积层厚度的影响。结果表明,在沉积层厚度一定的情况下,随基岩断层的滑动,沉积层中围绕断层投影线逐渐形成一个变形带以及由张性破裂和剪切破裂组成的破裂带,基岩断层的位移越大,沉积层中的变形带越宽、变形越强烈;但当基岩断层位移超过某一临界值后,变形带宽度将保持稳定,只是变形随断层位移增加而更集中。对于同样的基岩断层位移,沉积层厚度越大,受基岩断层控制的变形破裂带越宽,即基岩断层的影响范围越大;但当沉积层厚度超过某一临界值时,沉积层的变形发生了变化,沉积层表面并不存在与基岩断层走向一致的变形带,而是发育了较大尺度、与基岩断层走向斜交的张剪性破裂带。实验结果意味着,临界断层位移和临界沉积层厚度对于确定隐伏断层发震产生的地表变形和破坏具有重要意义  相似文献   

4.
推算气温变化时不同深度地层的地温变化幅度,进而计算其引起钢管基岩标石的线性胀缩量,结果表明:温度变化对钢管基岩标石的高程和钢管基岩标石间高差的影响量是水准成果应用中必须加以考虑和排除的.  相似文献   

5.
郑文俊  钱家栋  田山  刘允秀 《地震》2007,27(2):81-88
通过对宝坻台地电阻率与当地降水量以及该台深、浅井水位观测资料的相关性计算,并结合该地区水文地质和构造背景的分析,对该台十余年来地电阻率观测出现的缓慢下降的原因进行了研究。结果表明宝坻台地电阻率的长期缓慢下降主要与地下基岩背斜溶岩裂隙储水构造的含水量减少有关,而每年下半时段由降水集中引起的浅水位变化对地电阻率的短期变化具有影响。  相似文献   

6.
对于封闭条件较好的基岩承压水,影响其水位变化的因素主要有大气压力、潮汐应力、降水产生的附加应力、构造应力和震源应力。在多种因素综合作用下,如何识别并定量或半定量地分离出非地震因素引起的水位变化,提取真正的地震信息,是地震预报研究的重要环节。 本文以江苏泰县苏10井为例,运用数学  相似文献   

7.
不同结构的岩石试件变形破坏与孔隙压力关系的实验研究   总被引:5,自引:0,他引:5  
车用太  纪辉 《地震》1995,(4):333-339
根据华北地区地震地下水位动态观测井的含水层岩性、埋深与承压水头大小等实际条件,对具有不同结构的四种岩性试件,在不同围压、初始孔隙压力、变形速率下,进行了变形破坏过程中孔隙压力变化特征的实验研究,探讨了岩性、结构、围压、初即孔隙压力,变形速率等因素对井水位映震特征的影响。  相似文献   

8.
水位是影响水准高差变化最为显著和普遍的因素,本文研究了晋7-1~#井水位变化对太原地震台水准高差的影响,分析了两者的相关性及年最大变化量的异同情况。结果显示,相关性、年最大变化量比值异常与山西地震带地震有较好对应。  相似文献   

9.
地下水位动态受降雨影响显著,且由于降雨的持续时间、强度和面积的不同,由降雨引起的水位变化形态也复杂多样。为了能直观地判别降雨对水位的影响,排除水位资料中降雨的影响成分,本文采用水位月变化量与降雨月累计值作相关分析后得到的余差值,作为水位微动态研究对象。选用与降雨关系分别为显著、一般、不相关的连江江南井、泉州局一号井、福州浦东井水位进行分析,结果显示水位月变化量均表现了高值异常,异常与地震时间的对应关系有3个震前异常,2个同震异常、1个震后效应、1个无震异常。  相似文献   

10.
孙毅  牛安福  任越霞 《内陆地震》2007,21(3):251-257
对二滩电站水库蓄水后水位变化与水库库区、水库外围地区地震活动性进行了对比研究,并利用攀枝花南山台形变观测资料与水库水位变化之间的相关性,研究了"水库-小震-变形-中强震"之间的关系。结果表明,在由水位变化引起的加卸载过程中,加载时段是外围地区中强地震的有利发震时段,而卸载达到年度最低水平时,库区内地震活动明显增强。水库首次蓄水引起变形最为剧烈,之后影响逐渐减弱。  相似文献   

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《国际泥沙研究》2014,(4):F0003-F0003
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14.
《国际泥沙研究》2014,(2):F0003-F0003
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15.
《国际泥沙研究》2014,(3):F0003-F0003
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A procedure for short-term rainfall forecasting in real-time is developed and a study of the role of sampling on forecast ability is conducted. Ground level rainfall fields are forecasted using a stochastic space-time rainfall model in state-space form. Updating of the rainfall field in real-time is accomplished using a distributed parameter Kalman filter to optimally combine measurement information and forecast model estimates. The influence of sampling density on forecast accuracy is evaluated using a series of a simulated rainfall events generated with the same stochastic rainfall model. Sampling was conducted at five different network spatial densities. The results quantify the influence of sampling network density on real-time rainfall field forecasting. Statistical analyses of the rainfall field residuals illustrate improvement in one hour lead time forecasts at higher measurement densities.  相似文献   

18.
The partitioning of rain water into throughfall, stemflow and interception loss when passing through plant canopies depends on properties of the respective plant species, such as leaf area and branch angles. In heterogeneous vegetation, such as tropical forest or polycultural systems, the presence of different plant species may consequently result in a mosaic of situations with respect to quantity and quality of water inputs into the soil. As these processes influence not only the water availability for the plants, but also water infiltration and nutrient leaching, the understanding of plant effects on the repartitioning of rain water may help in the optimization of land use systems and management practices. We measured throughfall and stemflow in a perennial polyculture (multi‐strata agroforestry), monocultures of peach palm (Bactris gasipaes) for fruit and for palmito, a monoculture of cupuaçu (Theobroma grandiflorum), spontaneous fallow and primary forest during one year in central Amazonia, Brazil. The effect on rain water partitioning was measured separately for four useful tree species in the polyculture and for two tree species in the primary forest. Throughfall at two stem distances, and stemflow, differed significantly between tree species, resulting in pronounced spatial patterns of water input into the soil in the polyculture system. For two tree species, peach palm for fruit (Bactris gasipaes) and Brazil nut trees (Bertholletia excelsa), the water input into the soil near the stem was significantly higher than the open‐area rainfall. This could lead to increased nutrient leaching when fertilizer is applied close to the stem of these trees. In the primary forest, such spatial patterns could also be detected, with significantly higher water input near a palm (Oenocarpus bacaba) than near a dicotyledonous tree species (Eschweilera sp.). Interception losses were 6·4% in the polyculture, 13·9 and 12·3% in the peach palm monocultures for fruit and for palmito, respectively, 0·5% in the cupuaçu monoculture and 3·1% in the fallow. With more than 20% of the open‐area rainfall, the highest stemflow contributions to the water input into the soil were measured in the palm monocultures and in the fallow. Copyright © 1999 John Wiley & Sons, Ltd.  相似文献   

19.
Red tide, a recurrent phenomenon has become conspicuous in several Kashmir lake ecosystems since 1991. The responsible organism (Euglena pedunculata), a rare flagellate rediscovered in the Kashmir Himalaya (Khan 1993) caused first and unprecedented red tide outbreak, constituting a maximum of 96% of resident numerical phytoplankton density in Dal Lake. At present, conflicting hypotheses exist on the generation of causal assemblage(s) imparting redness to waters: Jeeji Bai (1991) linked its origin to acid precipitation – a fallout of burning oil‐fields during the Gulf War – whilst Khan (1993) holds local factor(s) responsible. Field/experimental studies support the latter contention that the influx of untreated sewage, in unison with warm temperatures, high levels of PhAR, iron and interruption to hydrological flow‐pattern together with absence/or reduction in grazing activity created conducive environmental milieu for red tide outbreak. Dal Lake “red tide” drifted the bloom‐inoculum to other waters, including Lake Wular, where additional ecological niches were carved out, threatening the aesthetic value and biological diversity of Kashmir lakes. Ecological monitoring indicates frequent seasonal red tide occurrence in Dal Lake (including summer‐autumn event of 1998) which testifies its unabated eutrophication status. Further studies are needed on ecological adaptability and biogeographic distribution of this rare and unique red tide‐causing flagellate.  相似文献   

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