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171.
考虑含水率影响的非饱和原状黄土冻融强度试验研究 总被引:13,自引:0,他引:13
提出了用于非饱和原状黄土增湿的蒸汽增湿方法,给出了蒸汽增湿试验步骤,通过对比试验分析确定了适宜的试验参数,从增湿后水分分布是否均匀、土体密度是否改变等方面论证了蒸汽增湿方法的有效性。对含水率的测试结果表明,微波炉法测试结果能满足精度要求,酒精燃烧法在测试较高含水率时误差较大。进一步应用蒸汽增湿法得到的不同含水率原状土样测定了非饱和黄土冻融后的强度指标,揭示出当非饱和原状黄土含水率过低时,冻融作用对黄土的粘聚力值基本没有影响,当含水率较高时,经历冻融循环后黄土粘聚力值较冻融前降低,冻结温度越低以及冻融循环次数越多,降低值越大。经历冻融循环后黄土内摩擦角值较冻融前增加,冻结温度越低,增加值越大。在含水率较低时冻融循环次数几乎不引起内摩擦角值发生变化,在含水率较高时冻融循环次数越多,引起内摩擦角增加值越大。 相似文献
172.
针对青海一些地区盐渍土当硫酸钠含量小于1%时也会产生盐胀,而超氯盐渍土却不会产生溶陷的事实,进行了较为深入细致的论证和研究。以数据、事实为依据,得出了与现行理论及规范有较大出入的论断。 相似文献
173.
By combining the carbon cycle model with the records of carbonate and organic (kerogen) carbon isotope, this paper presents
the calculation of the fraction of organic carbon burial (f
org) of beds 23–40 at the global boundary stratotype section and point (GSSP) of the Permian-Triassic boundary at Meishan, Zhejiang
Province. The resulting calculation produces two episodes of f
org maxima observed to occur at beds 23–24 and 27–29, which respectively corresponds to the two episodic anoxic events indicated
by the flourish of green sulfur bacteria. Two episodic f
org minima occurred at beds 25–26 and 32–34, generally coincident with the flourish of cyanobacteria (bed 26 and upper part of
beds 29 to 34) as shown by the high value of 2-melthyhopnoanes. It appears that the f
org is related to the redox conditions, with greater f
org values observed under the reductive condition. The relationship between f
org and the total organic carbon (TOC) content was complex. The f
org value was low at some beds with a high TOC content (such as bed 26), while high observed at some beds with a low TOC content
(e.g. bed 27). This association infers the important contribution of primary productivity to the TOC content. The original
organic burial could be thus calculated through the configuration of the function of the primary productivity and f
org, which can be used to correct the residual TOC measured today. This investigation indicates that compiling the organic-inorganic
carbon isotopes with the carbon cycle model favors to understand the fraction of organic carbon burial, providing information
for the reconstruction of the coupling among biota, environments and organic burial.
Journal of China University of Geosciences, 2007, 32(6): 767–773 [译自: 地球科学—中国地质大学学报] 相似文献
174.
Zhu Qian Luo Yulin Zhou Dongyang Xu Yue-Ping Wang Guoqing Tian Ye 《Natural Hazards》2021,105(2):2161-2185
Natural Hazards - Droughts have caused many damages in many countries and might be aggravated around the world. Therefore, it is urgent to predict and monitor drought accurately. Soil moisture and... 相似文献
175.
Acta Geotechnica - Suffusion is a typical form of internal erosion for gravel soils in which fine particles are detached by seepage and transport by water through pores. The prediction of erodible... 相似文献
176.
Liu Li Li Yucheng Wu Yongkang Luo Shengmin Peng Jing Deng Yongfeng Zhang Guoping 《Acta Geotechnica》2022,17(11):5113-5132
Acta Geotechnica - The macroscale mechanical properties of cement-stabilized soil have been widely reported, but the microscale behavior remains largely unexplored. This paper presents the first... 相似文献
177.
大地形上空偶极子东移对热带气旋路径的影响 总被引:1,自引:0,他引:1
With a quasi-geostrophic barotropic model on the β-plane with a topography term, 16 experiments were performed with an integration period of 6 days. The interaction between tropical cyclone tracks and 500 kin-scale vortices originating from the western part ora large-scale topography is investigated. It is suggested that this kind of interaction may have a significant impact on the moving speed and direction of tropical cyclones. Under certain conditions, this interaction may be a factor in causing an abnormal tropical cyclone track. Furthermore, the effect of large-scale topography plays an important role in the formation of unusual tropical cyclone tracks. 相似文献
178.
179.
Luo Hongxi 《岩土力学》1987,8(2):29-36
In southern China, there are a great amount of red clay(laterite) which contains some free ferric oxide. Owing to its composition and microstructure developed under hot, wet soil-forming conditions, the clay has several special characteristics. Although the water content and void ratio of laterite are greater than similar clay soils, its strength is still higher than the others. There seems to be a contradiction between its physical parameters and mechanical properties. In this paper, the effect of free ferric oxide in laterite on its engineering properties, such as strength, swelling properties and others is discussed. The research result shows that special properties of laterite are the result of various conditions of formation, loss and crystallization degree of free ferric oxide, and its physical and mechanical properties will change with variation of physicochemical circumstance. 相似文献
180.
降雨及地下水对边坡稳定性动态影响的初步研究 总被引:8,自引:0,他引:8
论述了降雨及地下水对边坡稳定性的动态影响及作用特征。这种影响特征具有典型的周期性和滞后性,通过对坡体地下水位的动态模拟,取得了边坡稳定性随时间而变化的规律认识。 相似文献