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61.
62.
The 2010 Yushu earthquake triggered landslide hazard mapping using GIS and weight of evidence modeling 总被引:8,自引:3,他引:8
Chong Xu Xiwei Xu Yuan Hsi Lee Xibin Tan Guihua Yu Fuchu Dai 《Environmental Earth Sciences》2012,66(6):1603-1616
The Yushu County, Qinghai Province, China, April 14, 2010, earthquake triggered thousands of landslides in a zone between
96°20′32.9″E and 97°10′8.9″E, and 32°52′6.7″N and 33°19′47.9″N. This study examines the use of geographic information system
(GIS) technology and Bayesian statistics in creating a suitable landslide hazard-zone map of good predictive power. A total
of 2,036 landslides were interpreted from high-resolution aerial photographs and multi-source satellite images pre- and post-earthquake,
and verified by selected field checking before a final landslide-inventory map of the study area could be established using
GIS software. The 2,036 landslides were randomly partitioned into two subsets: a training dataset, which contains 80 % (1,628
landslides), for training the model; and a testing dataset 20 % (408 landslides). Twelve earthquake triggered landslide associated
controlling parameters, such as elevation, slope gradient, slope aspect, slope curvature, topographic position, distance from
main surface ruptures, peak ground acceleration, distance from roads, normalized difference vegetation index, distance from
drainages, lithology, and distance from all faults were obtained from variety of data sources. Landslide hazard indices were
calculated using the weight of evidence model. The landslide hazard map was compared with training data and testing data to
obtain the success rate and predictive rate of the model, respectively. The validation results showed satisfactory agreement
between the hazard map and the existing landslide distribution data. The success rate is 80.607 %, and the predictive rate
is 78.855 %. The resulting landslide hazard map showed five classes of landslide hazard, i.e., very high, high, moderate,
low and very low. The landslide hazard evaluation map should be useful for environmental recovery planning and reconstruction
work. 相似文献
63.
64.
扬子地块西南缘晚古生代基性岩浆岩的性质与古特提斯洋的演化 总被引:16,自引:1,他引:16
扬子地块西南缘晚泥盆世至晚二叠世的基性岩浆岩具有大体类似的地球化学性质, 它们均富集Ti(TiO2> 2% )、LILE和LREE(La/Yb)N= 4.8~14.6),Ti/V(32~67)、Ti/Y(400~693)和Zr/Y(3.2~7.6)比值高,具洋岛玄武岩的特征,推测它们均与地幔柱岩浆的活动有关。该地幔柱岩浆活动的时期与古特提斯洋盆演化的时期大体吻合, 但地幔柱岩浆开始喷发的中心与古特提斯初始扩张的中心相距甚远,看来,金沙江-哀牢山洋盆的张开与地幔柱岩浆活动无关。从晚泥盆世至晚二叠世,地幔柱岩浆活动的规模和强度逐渐增加,玄武岩分布中心从广西的南宁-百色之间逐渐向北西310°方向迁移了约600 km ,推测这一迁移轨迹可能受金沙江-哀牢山洋盆扩张的影响。据此估计, 金沙江-哀牢山洋盆宽度可达约1 000 km 。据地幔柱岩浆轨迹与金沙江-哀牢山缝合带所夹的角度推测, 扬子地块可能经历了顺时针旋转, 与古地磁资料一致。 相似文献
65.
Regulating Environmental Factors of Nutrients Release from Wheat Straw Biochar for Sustainable Agriculture 总被引:1,自引:0,他引:1
One mechanism by which biochar application enhances soil nutrient availability is through direct nutrients release from biochar. However, factors controlling the release processes are poorly understood. In this study, the effects of pH, biochar to water ratio, temperature, ionic strength, and equilibration time on the release of PO, NO, NH, K+, Na+, Ca2+, and Mg2+ from biochar were evaluated in simulated experiments. The release of PO, K+, Ca2+, and Mg2+ was significantly affected by extraction pH, suggesting that their release from biochar was pH dependent or an H+‐consuming process. Correlation analysis indicated that PO and Ca2+, PO and Mg2+, and Ca2+ and Mg2+ were co‐solubilized with increasing soil acidity. To a lesser extent, the recovery of the nutrients was also affected by the ratio of biochar to water: more nutrients were soluble with more water supply. In contrast, the release of Na was not affected by pH while the concentration increased with decreasing biochar to water ratio. Meanwhile, other factors (temperature, ionic strength, and equilibration time) had less effect on nutrient release from biochar. Under the influence of pH, the patterns of NO and PO release from biochar were different: extractable NO concentration was not affected by the pH but more PO was released in strongly acidic conditions. Our data suggested that P was mainly retained in inorganic forms while N was in organic forms in biochar. We conclude that environmental factors have marked influences on nutrients release from biochar. 相似文献
66.
动物代谢的主要能源物质为脂肪、碳水化合物和蛋白质,前两者在体内可以完全氧化而生成二氧化碳和水,而蛋白质的代谢终产物是氨、尿素和其它含氮化合物,它们是含能物质。鱼类蛋白质的含氮代谢物质主要通过鳃排出,少量通过尿液排出(Beamish et al.,1984),这种排泄物的能量损失也称为非粪便失能。
鱼类非粪便失能的测定方法主要是直接测定鱼的氨及尿素排泄量,然后通过氨及尿素的含能量来计算;另一种方法是通过氮收支方程来间接估计排泄物的能量损失(Gerking,1955;Savitz,1971; Savitz et al.,1977;Lwata,1970;Porter et al.,1987),Braaten(1979),Bower等(1980),Cameron等(1983), Brafield(1985)和Knights(1985)对鱼类排泄量的各种测定方法进行了介绍和综述。本研究是应用氮收支方法来间接估算黑鲷的排泄能损失。这对于探讨鱼类对蛋白质的利用效率及代谢产物对养殖水环境的影响都具有一定的指导意义。 相似文献
67.
Xu Yadong Guo Rongwei Yan Haodong Wu Pengcheng Yang Yu 《Geotechnical and Geological Engineering》2022,40(3):1213-1224
Geotechnical and Geological Engineering - Deep coals are generally in a high geothermal environment, and when UCG (underground coal gasification) is carried out, the long-term high temperature... 相似文献
68.
An experimental study has been carried out to determine the partition coefficients of tungsten between aqueous fluids and
granitic melts at 800 °C and 1.5 kb with natural granite as the starting material. The effects of the solutions on the partition
coefficients of tungsten show a sequence of P > CO
3
2−
> B > H2O. The effects are limited (generallyK
D
< 0.3) and the tungsten shows a preferential trend toward the melt over the aqueous fluid. The value ofK
D
increases with increasing concentration of phosphorus; theK
D
increases first and then reduces with the concentration of CO
3
2−
when temperature decreases, theK
D
between the solution of CO
3
2−
and the silicate melt increases, and that between the solution of B4O
7
2−
and the silicate melt decreases. The partition coefficients of phosphorus and sodium between fluids and silicate melts have
been calculated from the concentrations of the elements in the melts. TheK
D
value for phosphorus is 0.38 and that for sodium is 0.56. Evidence shows that the elements tend to become richer and richer
in the melts. 相似文献
69.
70.
Based on monitored data from 840 samples, we assessed the spatial and temporal variability of groundwater salinization in the Tarim River lower reaches combining classical statistics and geostatistics. Results show that total dissolved solids (TDS) is significantly correlated with other related ions, such as Na+, Mg2+, Ca2-, C1- and K+. TDS and underground water level have characteristics of spatial autocorrelation, both of which present the isotropic characteristic and con- form to the spherical model in each year from 2001-2009. TDS is basically greater than 1 g/L but less than 2 g/L in the Tarim River lower reaches, which indicates that salt stagnation pollution is more serious. The most serious salinization (3 g/L 〈 TDS _〈 35 g/L) contaminated area is mainly in the middle and lower part of the study area. 相似文献