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901.
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904.
Spatial variability of soil moisture content and its relation to environmental indices in a semi-arid gully catchment of the Loess Plateau, China 总被引:16,自引:0,他引:16
The degree of spatial variability of soil moisture and the ability of environmental attributes to predict that variability were studied at the Da Nangou catchment (3·5 km2) in the semi-arid loess area of China. Soil moisture measurements were performed biweekly at five depths in the soil profile (0–5 cm, 10–15 cm, 20–25 cm, 40–45 cm and 70–75 cm) from May to October 1998 and from May to September 1999 using Delta-T theta probe. Results indicated that with increasing soil depth, the mean soil moisture content increases significantly for five layers and the coefficients of variation (CV) also increases with depth from 10–15 cm. It was observed that heavier rains and higher mean moisture contents are often associated with lower spatial variability (CV). Environmental attributes such as land use and topography play controlling roles in the spatial distribution of soil moisture content. However, the relative roles of these environmental indices vary with soil depth. The dominant controls on spatial variability of the time-averaged soil moisture changes from land use, aspect, relative elevation and hillslope position in the surface soil (0–5 cm) to relative elevation, hillslope position and aspect in the subsurface soil (10–15 cm, 20–25 cm), and to land use, relative elevation and slope gradient at larger depths (40–45 cm, 70–75 cm). The dynamic behavior of influences of different environmental indices on the layer-averaged soil moisture depends on several factors. In general, the correlation of soil moisture with slope gradient shows a more significant increase following a greater amount of antecedent precipitation (except for the extremely heavy storms), and declines afterwards. The relation of soil moisture with relative elevation and hillslope position exhibits an opposite trend. It was observed that the influence of land use corresponds to the difference in vegetative characteristics, with a stronger influence in June and August with a greater difference in vegetation. A significant influence of cos(aspect) was found during early spring and autumn with a rapid transient in solar irradiation. Finally, it was found that the sample size is adequate to estimate the catchment mean soil moisture at all five depths and on all 10 observations in 1999 (81 sites), while it is only enough for the upper soil layers (0–5 cm and 10–15 cm) in 1998 (26 sites). 相似文献
905.
综合研究了福建省上地幔的矿物、岩石、地球化学、地球物理(重、震、电)等有关资料,全面论证上地幔B′与B″层的三维空间特征、可疑地幔岩性、古代与现代地幔岩岩石类型与矿物成分。继而从地幔岩矿物组合,化学成分、微观特征、包裹体、稳定同位素等特点,来探讨第三纪上地幔的成岩环境与动力学,并指出东南沿海岩石圈上地幔减薄斜坡带及其叠生的深切断裂是燕山期双系列岩浆岩形成的深部地质背景。 相似文献
906.
By the measurement of the wind directional indicator of the Cretaceous desert in Ordos Basin, the regularity of the paleoprevailing
wind directions and pattern of the paleowind belts are revealed. It is considered that the desert was controlled by a planetary
wind system. In the early stage, the subtropical high pressure zone drifted south and northwards with short cycles, resulting
in the alternation of westerlies and northeast trades; in the late stage, the subtropical high pressure zone drifted southwards
with a long cycle, placing the desert under the westerly belt and making the desert completely controlled by the westerly
belt. The reconstruction of the paleowind belts has provided the evidence of the general circulation of the atmosphere for
the pattern of the circulation before the uplift of the Tibetan Plateau 相似文献
907.
对1966年3月8日邢台6.8级地震后的异常进行了逐项分析与讨论,发现有些震后异常与后续7.2级主震有比较可信的内在联系。本文在归纳邢台震后异常特征的基础上,提出了6条可能在同类条件下对预报后续地震具有普遍意义的意见。 相似文献
908.
地震灾害快速评估的计算机方法和程序 总被引:4,自引:0,他引:4
文中介绍一种在微机上实现的地震灾害快速评估应用软件:DISEV,DISEV由地震输入系统,图形显示系统,灾害评估系统和数据输出系统等4部分组成,采用确定性的地震灾害评估方法,用C语言设计完成,DISEV操作简单,快速,对震后快速反应工作以及救灾工作有重要意义。 相似文献
909.
In the present paper, the boundary element method with exterior collocation was applied to two-dimensional elastodynamic problems. The stability of the numerical solution was discussed and the collocation rule of source points outside the region being studied was investigated in the frequency domain by means of the computed error in the boundary displacement and the condition number of the coefficient matrix for two typical wave propagation problems. The achieved results are helpful to the practical application of this method to earthquake ground motion analysis. 相似文献
910.