共查询到20条相似文献,搜索用时 411 毫秒
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1995年3月19日,新疆和硕县那音克乡发生Ms5.0级地震。震前,乌鲁木齐地区地下水中溶解气体Ar、CH4、CO2、H2S等和库尔勒地区的断层气Rn相继出现明显的异常。异常具有短期临震性质,主要表现为短期趋势升高,临震突跳。 相似文献
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对滇西地震预报实验场多年来观测的Ar、N2、CO2等断层气体及水氡数据进行了分析,发现与朔望月密切相关的13.4-15天及27.7-30天周期。它是断层气体的潮汐响应,可称之为“断层气体潮”。这为研究地震异常提供了一项新的对比标准。 相似文献
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地壳中的CO2及其释放与地震短临预测 总被引:5,自引:0,他引:5
该文通过对地壳中二氧化碳(CO2)的分布及其与多震层的关系,以及地壳中CO2的释放与地震活动关系的分析,探讨了断层带CO2监测在强震短临预测阶段对时间判定的作用,提出应进一步加强对断层带CO2释放的监测与研究。 相似文献
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断层气CO2快速测定法及其在地震研究中的应用 总被引:1,自引:0,他引:1
自八十年代起,国内外地震工作者开始重视断层气的研究。近年来,我国在这方面的研究已获得了很大的进展。有关资料表明,CO2的释放与断裂活动性关系密切,它也是地震前兆的灵敏组分之一。总之,CO2是一种对地壳应力反映灵敏的气体地球化学指标,目前已被广泛应用于地震科学研究之中。就测定CO2的技术方法而言,当前国内餐主要利用气相色谱仪测定。由于气相色谱仪比较昂贵,且操作复杂,需配备具有较高素质的技术人员,所以 相似文献
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总结了对1996年2月3日云南丽江7级地震的中短期监视及跟踪预报过程。根据川滇地区地震活动特征和可公度性计算结果,在该次地震前对大形势进行了预测。1995年10月以后,滇西北地区出现了大面积、大幅度、多手段的同步异常,其中以水氡 、水位和CO2异常为主,沿中甸-南涧的地震区分产为集中。根据上述异常特征及异常分布情况,作在该次地震前2个同大理州政府提出了书面预报意见,认为1996年2月底以前在中甸 相似文献
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M. N. French R. L. Bras W. F. Krajewski 《Stochastic Environmental Research and Risk Assessment (SERRA)》1992,6(1):27-45
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
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Gtz Schroth Luciana Ferreira Da Silva Marc‐Andree Wolf Wenceslau Geraldes Teixeira Wolfgang Zech 《水文研究》1999,13(10):1423-1436
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
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M. A. Kahn 《洁净——土壤、空气、水》2000,28(2):95-101
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