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101.
Static uniaxial compression tests were conducted on 16 granite specimens after thermal treatment using a heating device and an electro-hydraulic servo pressure-testing machine. The effects of air cooling and water cooling on the physical and mechanical properties of the high-temperature granite specimens were studied. Test results showed that the longitudinal wave velocities of the high-temperature specimens gradually decreased after they were cooled by water and air. The peak stress and elastic modulus of the samples decreased gradually with an increase in temperature, whereas their peak strain increased gradually. The effects of peak stress and peak strain were considerably more evident when cooling by water than by air. This result demonstrated that the thermal cracking of the granite specimens, and consequently, their internal micro-fractures, further developed when the specimens were cooled by water. 相似文献
102.
YANG Weifeng CHEN Min . CAO Jianping QIU Yusheng ZHANG Run MA Qiang TONG Jinlu YANG Junhong YANG Zhi L U E 《海洋学报(英文版)》2009,(2):45-53
Thorium-234 and particle composition (organic matter, biogenic silica, carbonate and lithogenic component) were examined in the East China Sea (ECS) and the northern South China Sea (NSCS) in order to constrain the particle types scavenging thorium isotopes. Good positive correlations between particulate organic matter (POM) or carbonate and thorium-234 in suspended particulate matter (SPM) indicates that POM and carbonate are e.cient to scavenge thorium-234. No relationship between biogenic silica and thorium-234 suggests that geochemical behavior of thorium-234 may be not in.uenced by biogenic silica. A simple model was used to evaluate the a.nity of thorium-234 to di.erent particle components. The results show that POM is the most e.cient scavenger for thorium-234 in the ECS and the NSCS, followed by carbonate. The authors’ results lend support to the utility of thorium-234 as a proxy of POC and carbonate in the upper layer. However, the strong dependence of thorium scavenging on particle composition challenges thorium-230 as a constant .ux proxy. 相似文献
103.
湖相碳酸盐岩是一种分布极其广泛的陆相碳酸盐岩。中国湖相碳酸盐岩沉积始于二叠纪—三叠纪,经侏罗纪—白垩纪发展,鼎盛于古近纪,具有沉积时间跨度长、分布面积广的特征。碳酸盐岩发育方式多样,常以多个单层、薄夹层状、互层状、韵律沉积为主,也见以结核状或钙质微体化石等薄层赋存于泥岩、页岩等细粒碎屑岩中。湖相碳酸盐岩δ13C值介于-10.0×10-3~+10.0×10-3之间,多数为-5.0×10-3~+5.0×10-3,正负值均有。二叠系—三叠系δ13C发生负偏,侏罗系—白垩系先正向漂移随后负偏,古近系—新近系再次正偏,达最大值约+5.0×10-3。氧同位素δ18O值介于-20.0×10-3~+2.0×10-3之间,多数为-15.0×10-3~-0.0×10-3,几乎全部为负值。二叠系—三叠系、侏罗系—白垩系碳酸盐岩δ18O值在-15.0×10-3~-3.0×10-3之间变化,古近系—新近系δ18O值明显正偏移,多数位于-10.0×10-3~0.0×10-3。中国湖相碳酸盐岩碳氧同位素相关性分析表明,δ13C与δ18O密切相关,且δ13C值多正值或轻微负值,指示湖泊为封闭型咸水—半咸水环境;δ13C和δ18O不相关,δ13C值为负值,指示湖泊为开放型淡水环境。 相似文献
104.
Trace element contaminations of roadside soils from two cultivated wetlands after abandonment in a typical plateau lakeshore, China 总被引:1,自引:1,他引:0
Junhong Bai Qinggai Wang Kejiang Zhang Baoshan Cui Xinhui Liu Laibin Huang Rong Xiao Haifeng Gao 《Stochastic Environmental Research and Risk Assessment (SERRA)》2011,25(1):91-97
Total concentrations of As, Cd, Cu, Ni, Pb and Zn were determined in order to assess their changes in contamination levels
in roadside soils of long-term abandoned tillage (LAT) belt and short-term abandoned tillage (SAT) belt from a plateau lakeshore
of China. Results showed that the mean concentrations of these trace elements except for Cd and Pb were lower than background
values. The contamination index values of these trace elements fluctuated and generally decreased with increasing distances
from the road in both sampling belts except for Cu and Ni. Both LAT and SAT soils were facing Cd and Pb contamination. The
integrated contamination level was more serious in LAT soils compared to SAT soils, with heavy contamination levels at the
distances from 5 to 10 m in LAT soils. The effects of the studied rural road on both belts were clearly shown up to 250 m
away from the road. 相似文献
105.
湖南慈利江垭剖面中 上二叠统自下而上可以分为栖霞组、茅口组、吴家坪组和大隆组,总厚度为4617 m。该剖面岩以石灰岩为主,含少量的硅岩、泥岩、页岩和白云岩。石灰岩进一步分为砾屑灰岩、砂屑灰岩、粉屑灰岩、生物碎屑粒泥灰岩以及生物碎屑泥粒灰岩。砾屑灰岩主要分布于栖霞组及茅口组中,为斜坡沉积作用的产物。白云岩主要为同生和准同生白云岩,为局限台地环境的产物。根据岩性、微相分析,可划分出滨岸、局限台地、开阔台地、台地边缘、斜坡及盆地6种沉积环境。沉积演化表明,研究区二叠纪发生了两次大规模的海侵,主要发生于栖霞期早期—茅口期晚期以及吴家坪期早期—长兴期晚期。值得指出的是,栖霞组及茅口组中斜坡沉积的发现,对于重新认识研究区中二叠世古地理分布、演化及斜坡的迁移具有重要的意义。 相似文献
106.
Soil nutrient distribution in two typical paddy terrace wetlands along an elevation gradient during the fallow period 总被引:1,自引:0,他引:1
Soil nutrient concentrations in the top soils from two paddy terraces were determined in order to investigate spatial distributions of soil nutrients along the elevations on the Yunnan plateau of China during the fallow period.Results showed that soil nutrients in both terraces were higher than the reference concentrations except for SOC,TN,TP and Fe.Soil macronutrients didn’t show significant differences in both terraces except for Mg and Ca,so did soil micronutrients except for Mn.Spatial distribution patterns of soil nutrients along the increasing elevations were different in both terraces.However,soil nutrients in both terraces were generally not significantly influenced by the elevations and soil pH values.The findings of this study can contribute to soil fertility management and ecological protection of Hani terraces. 相似文献
107.
108.
电离层延迟是合成孔径雷达差分干涉测量(DInSAR)的误差源之一,对长波段SAR数据影响尤为严重。文中提出联合SAR相位和振幅信息精确测量方位向偏移,并基于方位向偏移构建模型校正DInSAR电离层延迟相位。选取覆盖2008年汶川地震的ALOS PALSAR(轨道号471)同震干涉对为实验数据,进行电离层延迟校正实验和精度分析。结果表明,实验同震干涉对中电离层贡献相位达17rad,对应约32cm的视线向形变误差,经过校正后地震远场形变均方根减小59%。对比传统方法校正结果,所提方法可有效提高电离层延迟相位校正精度。 相似文献
109.
110.
The soil nitrogen dynamics in an inland salt marsh as affected by various experimental water levels 下载免费PDF全文
An 87‐day incubation experiment was conducted to investigate the effects of various water levels on the soil nitrogen content in an inland salt marsh of Xianghai, China. Soil samples were collected from depths in the range of 0 to 30 cm at 10‐cm intervals after 15, 54 and 87 days of incubation. The total nitrogen (TN), available nitrogen, nitrate nitrogen (NO3?‐N) and ammonium nitrogen (NH4+‐N) contents and the nitrogen activation coefficient (NAC) were measured to investigate the soil nitrogen dynamics under three inundation treatments (?5, 0 and 5 cm). The results showed that TN was generally accumulated in all soil layers and exhibited a peak value in subsurface soils at the ?5‐cm inundation level at the end of the incubation period, whereas no obvious changes were observed in the TN contents in the bottom soils at the three inundation levels. Compared with the initial contents in the soils, the NO3?‐N and NH4+‐N contents were significantly reduced in all soil layers at the 0‐cm and the 5‐cm inundation levels at the end of the incubation period. In general, the available nitrogen content was higher in the surface soils compared with the deeper soils at all inundation levels. The NAC values exhibited a pronounced change in the subsurface soils at all inundation levels, decreasing significantly from 0.17 to 0.04 at the 5‐cm inundation level; however, a higher mean NAC value (0.126) was found over the incubation period at the 0‐cm inundation level compared with the 5‐cm and the ?5‐cm inundation levels. Nitrogen was released from plants into the soil under all inundation treatments over the incubation period. The soil organic matter exerted positive loadings on the TN and NO3?‐N contents and negative loadings on the NH4+‐N content at all inundation levels, and the water content generally exhibited a negative relationship with all forms of nitrogen. Additionally, the total phosphorus content exhibited a positive correlation with the TN and NO3?‐N contents. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献