Analysis of microscopic pore structures of the silty clay before and after freezing–thawing under the subway vibration loading     

Zhong-Liang Zhang  Zhen-Dong Cui 《Environmental Earth Sciences》2017,76(15):528

With the rapid development of the subway rail transit, the effect of the cyclic loading on the surrounding foundations and buildings has drawn wide attention. In addition to the in situ tests and the laboratory triaxial tests, microscopic tests also provide an effective way to clarify the physical and mechanical characteristics of soils. On the other hand, the characteristics of the soft silty clay before and after freezing–thawing has been less studied. In this paper, the scanning electron microscope (SEM) tests following the cyclic triaxial tests of silty clay layer were performed to investigate the variations of the microscopic pore structures of the layer before and after freezing–thawing. The corrected Otsu method was used to obtain the binary SEM images of silty clay. The porosity results demonstrate that the magnifications from 1000× up to 5000× were suitable for observation of the silty clay microstructures. The binary SEM images of soil pore structures were quantitatively analyzed, including the porosity, the size distribution, the pore shape coefficient, the pore orientation distribution and the fractal dimension. The pore orientation of samples without loading is arranged in the horizontal direction, while the pores of samples under cyclic loadings are arranged in the vertical. After freezing–thawing, the mean anisotropy value of the microscopic pore structures increased about 12% and the porosity of samples without loadings increases about 11.24%. The lower the freezing temperature is, the larger the porosity within the samples becomes. However, the freezing–thawing has little effect on the pore shape coefficient of the silty clay. The porosity of the silty clay increases with an increase in pore diameter, but it decreases with the increase in excess pore pressure. In addition, the microscopic pore structures of the silty clay exhibit fractal characteristics. The fractal dimension is reduced by the disturbance from the effect of freezing–thawing, coupled with the effect of cyclic loading.  相似文献   

Estimating the contribution of glacial meltwater to Ranwu Lake,a proglacial lake in SE Tibet,using observation data and stable isotopic analyses   总被引：1，自引：0，他引：1  

Jianting Ju  Liping Zhu  Junbo Wang  Yingying Cui  Lei Huang  Ruimin Yang  Qingfeng Ma  Lun Luo  Yongjie Wang 《Environmental Earth Sciences》2017,76(5):229

It is important for both current monitoring and paleoenvironmental research conducted on proglacial lakes and their adjacent glaciers to clarify the hydrological processes operating on these lakes. However, in remote regions with limited accessibility it may be difficult to study hydrological processes by direct monitoring. In this study, we use measurements of stable isotopic compositions to trace the multiple water sources contributing to Ranwu Lake, a proglacial lake in south-eastern Tibet. Using stable isotopic data from precipitation, inflowing rivers and the lake water, a water and isotope mass balance modelling method was used to calculate the ratio of evaporation to input. Subsequently, using hydrological and climatic data for the outflow, the largest inflow and precipitation, other hydrological elements of the lake water balance were also calculated. The results demonstrate that the ratio of evaporation to inflow is as low as 0.009, the lowest value observed for the Tibetan Plateau, indicating that Ranwu Lake is a through-flow lake with a very short retention time. Glacial meltwater accounts for at least 55% of total runoff, the highest value observed for the Tibetan Plateau, indicating that the sediments of Ranwu Lake may have considerable potential for reconstructing variations in the activity of the local glaciers. Finally, we note that it may be inappropriate in this glacier-fed lake to use the intersection of the local meteoric water line with the lake water line for determining the isotopic composition of the input water, and this possibility must be carefully considered when stable isotope mass modelling is used in proglacial lakes.  相似文献   

Speciation analysis of arsenic compounds in seafood by ion chromatography-atomic fluorescence spectrometry     

Tingting Han  Hongwei Ji  Huixin Li  He Cui  Tian Song  Xiaojuan Duan  Qianlin Zhu  Feng Cai  Li Zhang 《中国海洋大学学报(英文版)》2017,16(3):455-460

Ion chromatography-ultra violet-hydride generation-Atomic Florescence Spectrometry was applied to detect 5 arsenic species in seafoods. The arsenic species studied include arsenobetaine(As B), arsenite(As(III)), dimethylarsinic acid(DMA), monomethylarsonic acid(MMA), and arsenate(As(V)), which were extracted from samples using 2% formic acid. Gradient elution using 33 mmol L~(-1) CH_3COONH_4 and 15 mmol L~(-1) Na_2CO_3 with 10 mL CH_3CH_2OH at pH 8.4 allowed the chromatographic separation of all the species on a Hamilton PRP-X100 anion-exchange column in less than 8 min. In this study, an ultrasound extraction method was used to extract arsenic species from seafood. The extraction efficiency was good and the recoveries from spiked samples were in the range of 72.6%–109%; the precision between sample replicates was higher than 3.6% for all determinations. The detection limits were 3.543 μg L~(-1) for As B, 0.4261 μg L~(-1) for As(III), 0.216 μg L~(-1) for DMA, 0.211 μg L~(-1) for MMA, and 0.709 μg L~(-1) for As(V), and the linear coefficients were greater than 0.999. We also developed an application of this method for the determination of arsenic species in bonito, Euphausia superba, and Enteromorpha with satisfactory results. Therefore, it was confirmed that this method was appropriate for the detection of arsenic species in seafood.  相似文献   

Experimental study on the moving characteristics of fine grains in wide grading unconsolidated soil under heavy rainfall     

Yi-fei Cui  Xiao-jun Zhou  Chao-xu Guo 《山地科学学报》2017,14(3):417-431

The initiation mechanism of debris flow is regarded as the key step in understanding the debris-flow processes of occurrence, development and damage. Moreover, migration, accumulation and blocking effects of fine particles in soil will lead to soil failure and then develop into debris flow. Based on this hypothesis and considering the three factors of slope gradient, rainfall duration and rainfall intensity, 16 flume experiments were designed using the method of orthogonal design and completed in a laboratory. Particle composition changes in slope toe, volumetric water content, fine particle movement characteristics and soil failure mechanism were analyzed and understood as follows: the soil has complex, random and unstable structures, which causes remarkable pore characteristics of poor connectivity, non-uniformity and easy variation. The major factors that influence fine particle migration are rainfall intensity and slope. Rainfall intensity dominates particle movement, whereby high intensity rainfall induces a large number of mass movement and sharp fluctuation, causing more fine particles to accumulate at the steep slope toe. The slope toe plays an important role in water collection and fine particle accumulation. Both fine particle migration and coarse particle movement appears similar fluctuation. Fine particle migration is interrupted in unconnected pores, causing pore blockage and fine particle accumulation, which then leads to the formation of a weak layer and further soil failure or collapses. Fine particle movement also causes debris flow formation in two ways: movement on the soil surface and migration inside the soil. The results verify the hypothesis that the function of fine particle migration in soil failure process is conducive for further understanding the formation mechanism of soil failure and debris flow initiation.  相似文献   

Estimation of ecological water requirements based on habitat response to water level in Huanghe River Delta, China   总被引：3，自引：0，他引：3  

Baoshan Cui  Yanyan Hua  Chongfang Wang  Xiaolin Liao  Xuejie Tan  Wendong Tao 《中国地理科学(英文版)》2010,20(4):318-329

In recent years,wetland ecological water requirements (EWRs) have been estimated by using hydrological and functional approaches,but those approaches have not yet been integrated for a whole ecosystem.This paper presents a new method for calculating wetland EWRs,which is based on the response of habitats to water level,and determines water level threshold through the functional integrity of habitats.Results show that in the Huanghe (Yellow) River Delta water levels between 5.0 m and 5.5 m are required to maintain the functional integrity of the wetland at a value higher than 0.7.One of the dominant plants in the delta,Phragmites australis,tolerates water level fluctuation of about ± 0.25 m without the change in wetland functional integrity.The minimum,optimum and maximum EWRs for the Huanghe River Delta are 9.42×106 m3,15.56×106 m3 and 24.12×106 m3 with water levels of 5.0 m,5.2 m and 5.5 m,corresponding to functional integrity indices of 0.70,0.84 and 0.72,respectively.A wetland restoration program has been performed,which aims to meet these EWRs in attempt to recover from losses of up to 98% in the delta's former wetland area.  相似文献   

可压缩层流边界层系统的一些性质     

杜翠  罗圆 《成都信息工程学院学报》2010,(6):324-327

进一步研究了可压缩流边界层系统解的一些性质,给出了可压缩边界层系统等价的奇异积分方程解存在时参数所在的区间,并通过研究等价的奇异积分方程解的性质,得出可压缩层流边界层系统给出剪应力函数厂和温度函数g的一些结果．  相似文献   

The effect of toxic sulfide exposure on oxygen consumption and oxidation products in Urechis unicinctus (Echiura: Urechidae)     

KANG Kyoung Ho 《中国海洋大学学报(英文版)》2010,9(2):157-161

To investigate sulfide detoxification in Urechis unicinctus,oxygen consumption rate and sulfide detoxification productswere analyzed during sulfide exposure under controlled laboratory conditions.The results showed that oxygen consumption rateswere elevated significantly during 3 h sulfide exposure compared to the control(P0.05).The concentration of sulfite in body walland hindgut of experimental worms increased significantly(P0.05)when exposed to 50μmolL-1sulfide,reached a maximum at24 h and then decreased.Similar result was observed in worms exposed to 150μmolL-1sulfide except that sulfite concentrationreached a maximum at 12 h.Contents of thiosulfate in body wall and hindgut of U.unicinctus exposed to sulfide were also significantly higher than that of the control without sulfide exposure.In conclusion,during short-time sulfide exposure U.unicinctus mayraise oxygen consumption to detoxify toxic sulfide into sulfite and thiosulfate.Sulfide detoxification was restrained when the expo-sure time was prolonged or sulfide concentration was increased,which was indicated by decrease of sulfite,the intermediate productof sulfide detoxification.  相似文献   

Determination of Ca,K, Mg and Fe in four fish species by FAAS     

Xiaoli Cui  Yijun Wang  Xilin She 《中国海洋大学学报(英文版)》2010,9(3):235-238

A method for determining calcium(Ca),potassium(K),magnesium(Mg) and iron(Fe) in four fish species was optimized and validated.It included microwave mineralization of the samples and subsequent quantification by flame atomic absorption spectroscopy(FAAS) with Zeeman-effect background correction.Using HNO3(65%) and H2O2(33%) as extraction solutions,the optimal conditions of extraction were established as follows:0.5 g of sample mass;microwave time program of 300 W/5 min and 600 W/5 min.The method was free of matrix interferences.The linear correlation coefficients were ≥0.9991,the recovery percentage of analytes was from 99.31% to 103.70% and the RSD(relative standard deviation) was lower than 2.06%.The detection limits obtained were 32.3,43.2,14.0 and 68.6 ng mL-1 for Ca,K,Mg and Fe in FAAS respectively.It is shown that the method is rapid,simple,sensitive and accurate.The method was applied to the studies of digestibility and measurement of these nutrients in samples of fish collected from Norway,Japan and China.  相似文献   

Initiation and development of water film by seepage   总被引：1，自引：1，他引：0  

Xiaobing Lu  Peng Cui  Kaiheng Hu  Xuhui Zhang 《山地科学学报》2010,7(4):361-366

When water seeps upwards through a saturated soil layer,the soil layer may become instability and water films occur and develop.Water film serves as a natural sliding surface because of its very small friction.Accordingly,debris flow may happen.To investigate this phenomenon,a pseudothree-phase media is presented first.Then discontinuity method is used to analyze the expansion velocity of water film.Finally,perturbation method is used to analyze the case that a water flow is forced to seep upwards through the soil layer while the movement of the skeleton may be neglected relative to that of water.The theoretical evolutions of pore pressure gradient,effective stress,water velocity,the porosity and the eroded fine grains are obtained.It can be seen clearly that with the erosion and redeposited of fine grains,permeability at some positions in the soil layer becomes smaller and smaller and,the pore pressure gradient becomes bigger and bigger,while the effective stress becomes smaller and smaller.When the effective stress equals zero,e.f.liquefaction,the water film occurs.It is shown also that once a water film occurs,it will be expanded in a speed of U(t)(1-ε).  相似文献   

Characteristic rainfall for warning of debris flows   总被引：4，自引：2，他引：2  

Kaiheng Hu  Peng Cui  Chuanchang Wang  Yong Li  Xiaobing Lu 《山地科学学报》2010,7(3):207-214

A characteristic rainfall is introduced to overcome the difficulties encountered in determining a critical rainfall value for triggering debris flow.The characteristic value is defined as the rainfall at which debris-flow occurrence probability shows a rapid increase,and can be used as a warning rainfall threshold for debris flows.Investigation of recorded debris flows and 24-hour rainfall data at Jiangjia basin,Yunnan Province,in southwestern China,demonstrates the existence of such a characteristic rainfa...  相似文献