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2011 Vol. 30, No. 3

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Academic research and contributions on karst made by Academician Lu Yaoru
XIONG Kang-ning, LIU Qi, XIAO Shi-zhen
2011, 30(3): 243-247. doi: 10.3969/j.issn.1001-4810.2011.03.001
Abstract:
Lu Yaoru, an academician of Chinese Academy of Engineering, has been devoting all his life on the research on karst geology since 1950s. He carried out a systematic research on karst development regulations especially on the compounded karst processes and mechanism of karstification developed in sulphate and carbonate rocks. He also contributed much on hydrological, engineering and environmental geology issues in karst areas. He took part in and gave much guidance for exploratory studies on hydraulic and hydroelectric engineering, including hundreds of hydro-junction projects, such as the Three-gorge Dam, Wujiangdu Reservoir, and Xin’anjiang hydropower station, etc, in Yangtz River, Yellow River, Zhujiang River and Huaihe River catchments. He was also involved in study on engineering geology and environmental geology exploration referring transportation, towns and mines. Professor Lu advanced various hydrodynamic conditions, the mechanism of three-phase flow relations, mixed corrosions etc. In addition, he introduced new concepts including geo-ecological environment, rocky desertification and made the suggestions to develop research on these fields and the control of geological disasters in karsts areas. Professor Lu established a systematic theory on the karst development and its engineering effect, making great contribution to karst development and disaster prevention and control.
Influence of the May-12 Wenchuan Earthquake on hydro geochemistry of the source spring at the Huanglong World Heritage Site: Evidences from high resolution and high precision monitoring of hydro geochemistry
LIU Zai-hua, WANG Hai-jing, LIU Yan, TAI Yong-dong, FU Ru-xian, WANG Xiao-ping
2011, 30(3): 248-252. doi: 10.3969/j.issn.1001-4810.2011.03.002
Abstract:
The May-12 Wenchuan Earthquakein 2008 has not only huge injuries, casualties and economic losses but also serious impacts on the local eco-environment. Based on the high resolution and high precision monitoring results of hydro geochemistry obtained from the NSFC-supported project“Investigation on the mechanisms of anthropogenic and natural impacts on the decline of the travertine landscape at Huanglong the World Natural Heritage Site”, it was found that the great earthquake has remarkable influences on the hydro geochemistry of the Huanglong source spring, which recharges the Huanglong travertine-deposition stream. The influences mainly reflected in the increase in discharge, water temperature and electric conductivity as well as pCO2 of the spring, indicating the increase in fluxes of discharge, heat, calcium ion and CO2 towards the surface. However, the effect of the earthquake on the travertine landscape and CO2 release to the atmosphere remains to be assessed.
Distribution features of karst water in Yunnan
WANG Yu, PENG Shu-hui
2011, 30(3): 253-259. doi: 10.3969/j.issn.1001-4810.2011.03.003
Abstract:
Distribution features of karst water in Yunnan Province are summarized as follows. The karst aquifer is the comparatively homogeneous medium in the karst plateau plain. While it is the comparatively inhomogeneous medium on the edge of the karst plateau plain and the slopes of river valley. The aquifer characteristic of the karst catchment basin is same to the porous medium. In the catchment-runoff karst graben basin, water content is comparatively homogeneous in the upstream section but quite inhomogeneous in the karst cave and conduit in the downstream section. Furthermore, the water table of the saturated zone is nearly equivalent to the drainage spring in the identical hydro geologic unit. Generally, the karst stratum is mainly similar to the permeable bed in the recharge area and is nearly equal to aquifer in the runoff area and real aquifer in the discharge area. The features of the karst geomorphologic landscape could open out the enrichment situation of karst water. Moreover, the enrichment effects of water-storing structure are more important.
Comparative study on karst ground water simulation between GM(1, 1)decomposition model and ARIMA model: A case study on discharge simulation of the Liulin Spring
LI Hua-min, WU Jing, ZHAO Jiao-juan, HAO Yong-hong, WANG Ya-jie, CAO Bi-bo
2011, 30(3): 260-269. doi: 10.3969/j.issn.1001-4810.2011.03.004
Abstract:
The discharge of the Liulin spring is simulated with GM(1,1) decomposition model and ARIMA model respectively. According to the hydrological characteristics, the Liulin spring flow series could be divided into two periods. First, from 1957 to 1973 the spring flow was under natural state; second, from 1974 to 2009 the spring flow was impacted by both climate change and human activities. Using the data of first period, the spring flow under the natural state is fitted with GM(1,1) decomposition model and ARIMA model, and then the models are extrapolated to obtain the second periods’spring flow under the natural state. According the water balance principle, the spring flow decrement contributed by human activities is acquired by subtracting the observed discharge from simulated spring flow of the second period under the natural state. Thus, it is differentiated the effects of human activities from climate change. The simulated Liulin Springs’attenuation from 1970s to early 21st century is 2.26 m3/s by GM(1,1)decomposition model and 2.36 m3/s by ARIMA model with the relative error being 0.44% and 2.20% respectively, showing both GM(1, 1)decomposition mode land ARIMA model are suitable for spring flow simulation. Comparing the effects of human activities and climate change to the depletion of the Liulin Spring’s discharge, the authors find that the contribution of human activities is 8 to 9 times higher than that of the climate change. The empirical studies have shown that the GM (1,1) model is of high precision in simulating the exponential series. It can also improve accuracy by periodic amendment, when simulate the spring flow with periodic fluctuations. ARIMA model could reflect time-lag between precipitation and spring discharge and accurately simulate their quantitative relation.
Application of Visual Modflow in predicting shaft water inflow in the Baijian iron mining area
FENG Geng-chen, HAO Jun-jie, TAN Jun, XU Su-juan
2011, 30(3): 271-277. doi: 10.3969/j.issn.1001-4810.2011.03.006
Abstract:
Based on the analysis on hydrogeology and boundary conditions of the Baijian mining area, Visual Modflow model is recognized and verified with actual measurement data, meanwhile, the parameter of the aquifer is modified. The modified model is reliable and can be used for water inflow prediction in the Baijian mining area. According to the different boundary and permeability coefficient in the Ordovician limestone aquifer, three predicting schemes on -200m and -400m horizontal plane with different boundaries and permeability coefficients are designed and used. The results show that schemes 2 is more reasonable and can really reflect the water inflow when the water table drops down to -400m in Baijian mining area, and the predicted water inflow is 7505 m3/h.
The geophysical prospecting technique in different aquifer media in karst area, Southwest China
WU Yi, SUN Yin-hang, LI Feng-zhe
2011, 30(3): 278-284. doi: 10.3969/j.issn.1001-4810.2011.03.007
Abstract:
In this paper, based on the characteristics of groundwater occurrence in different media such as epikarst water, pipeline karst water (caves, underground rives, pipelines, etc.)and structural fissure karst water in Southwest China karst area, the applicability of geophysical methods and the characteristics of water detection are analyzed. And the geological problems in detecting water in different media with geophysical methods and integrated geophysical methods are put forward, and the response characteristic of electrical parameters(or curve)of those methods is summarized. Then the combination program of geophysical methods in different aquifer media is established. Finally, the usefulness of the program is verified and the technique experiences of geophysical prospecting for groundwater in Southwest China karst area are acquired.
Study on the situation and evolution trend of karst water pollution in Xingtai City
DU Wen-tang, WANG Zhan-hui, FENG Geng-chen, LI Shu-wen, ZHANG Jing-sen
2011, 30(3): 285-290. doi: 10.3969/j.issn.1001-4810.2011.03.008
Abstract:
Surface water pollution and solid waste disorderly piling up have led to contamination of karst groundwater in many places in Xingtai City and the polluted scope is continually enlarged, which is severely threatening water safety in downstream. On the basis of a large number of water quality monitoring data, the pollution situation of karst water was analyzed, two tendencies of groundwater pollution are predicted by means of numerical method under the circumstance of the polluting sources being controlled or the polluting sources still existing, and the impact of water pollution on water source is analyzed too. Predictions indicate that, if polluting sources still existing, the isoline of out of limits Cr6+ concentration will diffuse at the speed of 0.769 m/d; if polluting sources being controlled, the diffusing speed will reduce to 0.402 m/d. So, it thus clear that polluting sources treatment is of important role to slow down the diffusion of contaminants. The predicted results can be chosen as the basis for groundwater protection and pollution control.
Discharge estimation in the Shuangyanjing Spring small watershed in Fuquan, Guizhou and the solution of flood water release
ZHONG Jin, DONG Yu, DING Jian-ping
2011, 30(3): 291-294. doi: 10.3969/j.issn.1001-4810.2011.03.009
Abstract:
As a typical karst peak-cluster depression non-enclosed basin, the Shuangyanjing spring small watershed is 0.636 km2 in area. It is mainly recharged by precipitation through karst slocker and fissuring, and characterized by larger changing discharge with a range of 0.2~35.5 L/s. Flood peak flow calculation is inaccurate that threatening the safe operation of flood drainage engineering due to the inconsistent between surface watershed and underground watershed of karst aquifer. In order to solve the problem of lacking in long-term observation data for flood control project, this paper calculate the peak discharge as 27.5 L/s considered water-resisting layer as underground water catchment’s bound and used locate largest runoff modulus in high flow period, through karst hydrgeologic survey in the Shuangyanjing spring watershed. Then multiply the peak discharge by safety factor to get the data for wetted cross-section design. In light of the calculate results, it is suggested that to build a new retaining dam at altitude 940 m at the mouth of the Shuangyanjing valley to retain groundwater flood runoff and ease water discharge pressure in flood season.
Study on volume fractal features of soil particle under different land use types in southeast karst mountain of Chongqing
XIONG Bo, WANG Jian-li, ZHANG Tian-wen, SONG Jiang, LI Yan-jun
2011, 30(3): 295-301. doi: 10.3969/j.issn.1001-4810.2011.03.010
Abstract:
Through field survey, sampling and laboratory analysis on soil grain size in southeast karst mountain of Chongqing, by means of soil particle volume fraction dimensional model the soil particle volume fractal dimension characteristics of the arable land soil and abandoned land soil are analyzed. Then the relationship of the soil particle volume fractal dimension characteristics and particle volume content are discussed. The results show that the soil particle volume fractal dimension and the content of soil clay particle(<0.002 mm)is significant linear correlation, which proves that the more clay soil contain, the higher fractal dimension it is. And the relationship between the content of clay particle and the soil particle volume fractal dimension in the soil profile under different land use types show the same change rule. The fractal dimension of soil is not only affected by clay particle content but also by the homogeneity of soil texture. The fractal dimension of soil texture shows certain correlation with uniform index, but the association is relatively weak. The fractal dimension of arable land soil (mean 2.5065) is greater than that in the abandoned land (mean 2.4835), indicating that the impact of human agricultural activities on soil texture, especially on clay content, is obvious. Soil volume fractal dimension can serve as a regional indicator for arable land soil quality assessment.
Discussion on distribution and land utilization pattern of karst hill in Guangdong Province
WEI Xing-hu, LEI Li, XU Xi-zhen
2011, 30(3): 302-307. doi: 10.3969/j.issn.1001-4810.2011.03.011
Abstract:
The area of karst hill in Guangdong Province is 1827 km2, the karst hill is vital to agriculture and environmental protection. In this paper, based on the field investigation and data analysis, we discussed the distribution region, area, features, land utilization status and problems of four kinds of the karst hill, including low corrosion hill, low corrosion-erosion hill, high corrosion hill and high corrosion-erosion hill in Guangdong Province. The results show that the distribution of karst hill in Guangdong Province is broad and scatter, they main locate in the north and west of Guangdong Province, account for 76% and 19%, respectively. There are many problems in utilization of karst hill such as disforestation and planting fruit tree as well as planting eucalyptus. For prevent karst environment from irrational exploitation, we suggest5 kinds of land utilization patterns for different area as follows. Ecologic forest + economic forests + economic crop in karst basin area, ecologic forest + firewood forests + economic plant in karst plateau area, corrosion-erosion hilly area-fast growing timber stands, ecotourism, mine area-ecological forest + mineral resources exploitation in karst beauty spot.
Altitudinal distribution patterns of plant functional group biodiversity in Longhushan, Guangxi
LIANG Ming-zhong, JIANG Zhong-cheng, SHEN Li-na, XU Shu-qing
2011, 30(3): 308-312. doi: 10.3969/j.issn.1001-4810.2011.03.012
Abstract:
The biodiversity of plant community and evergreen plant functional group as well as deciduous plant functional group is investigated by means of belt transect method along altitudinal gradient in the Longhushan in Guangxi. Altitudinal distribution pattern analysis shows that the α-biodiversity has no obvious change with elevation in the arborous layer, but there is obvious difference between evergreen plant functional group and deciduous plant functional group and little difference between evergreen plant functional group and biodiversity of plant community; the β-biodiversity altitudinal distribution pattern is similar among community and evergreen plant functional group as well as deciduous functional group. Plant species diversity altitudinal distribution pattern is resulted from comprehensive effect by environmental factors and different response of functional groups. The impact of landform and lithology on biodiversity is studied in the article. The results show that the α-biodiversity altitudinal gradient distribution pattern is in accordance with the landform, but does not change with lithology obviously; the β-biodiversity altitudinal gradient distribution pattern is in accordance with lithology, but does not change with the landform obviously.
Impact of mycorrhizal fungus on the growth and nutrient absorption of Cupressus duclouxiana Hichel seedlings under water stress
WANG Ru-yan, YU Shui-qiang, ZHANG Jin-chi, CONG Ri-liang, WANG Qun, CHEN Li-sha, SI Deng-yu
2011, 30(3): 313-319. doi: 10.3969/j.issn.1001-4810.2011.03.013
Abstract:
The potted seedlings of Cupressus duclouxiana Hichel were tested to study their response characteristics under three different moisture content conditions, normal moisture(25~30%), moderate drought(15~20%) and severe drought(5~10%). Accordingly, the test include four inoculated groups, control group (A), VAM group (B, inoculated VAM), ectomycorrhizal(C, inoculated Ectomycorrhiza) and mixture group (D, VAM + Ectomycorrhiza). The biomass, root morphology and nitrogen content, phosphorus content of Cupressus duclouxiana Hichel seedlings were measured after 150 days. The results show that when the seedlings were inoculated with mycorrhizal fungus under normal moisture, the plant biomass was increased, including above-ground biomass and under-ground biomass. The effect to the contents of nitrogen and phosphorus was mainly on the root. The nitrogen content of roots was respectively increased significantly, by 65.4%, 118.2% and 117.7% in B, C and D group under normal moisture, respectively. The root phosphorus content of C and D group was obvious increased 40.4% and 49.4% compare to control group. The effect to root morphology was also significant, the D inoculated treatment were higher than that in controlled treatment on root length and surface area. Under mediate drought, there was significant difference among B, D and A in N content in roots, but significant difference among C, D and A in leaves. And there was significant difference among C, D and A in P content in roots and leaves. The trend of positive effect to root morphology was D> C> B> A. Under severe drought condition, the mycorrhizal fungi did not affected the plant biomass and nutrient content as well as root morphology. In brief, except for under severe drought condition, the mycorrhizal fungi would improve nutrient absorption and increase the biomass and benefit for enhancing survival rate of C. duclouxiana Hichel.
The hierarchy effect of settlement pattern evolution and its relationship with the traffic conditions in Karst mountain: A case study in Houzhaihe, Wangjiazhai and Maolan, Guizhou
LUO Guang-jie, LI Yang-bing, WANG Shi-jie
2011, 30(3): 320-326. doi: 10.3969/j.issn.1001-4810.2011.03.014
Abstract:
The settlements in the study area Houzhaihe, Wangjiazhai and Maolan are divided into 5 ranks according to space scale with high resolution images (in 1963, 1980s and 2004) and GIS analysis. The evolution discipline of the settlement’s distribution pattern and its relation ship with traffic conditions are discussed in the paper. The results show that, (1) there are less high-rank settlement but more low-rank settlement in 1963. The high-rank settlement mainly distributes in peak-forest plain where have more water and plow land resources; (2)from 1963 to 1980s, the development of settlement in karst mountain mainly focuses on middle rank settlements, high and low rank settlements barely changed; (3)by 2004, the number and scale of all settlements have developed substantially, but the strength of development is bigger in the two poles(rank 1 and rank 5); (4)change in settlement rank is not only influenced by traffic conditions, but also subjected to regional economic development level and physical geography environments in karst mountain area; (5)in the future, the reconstruction of the settlement and the improvement of traffic should be focused on rank 4 settlements, but space migration toward the road sides should be done for rank 5 settlements in order to improve accessibility.
The distribution characteristics of the epikarst reservoir in Lunnan Ordovician buried hill
CHEN Li-xin, PAN Wen-qing, LIANG Bin, LUO Ri-sheng, ZHANG Qing-yu, GAO Xiang
2011, 30(3): 327-333. doi: 10.3969/j.issn.1001-4810.2011.03.015
Abstract:
Lunnan ancient buried hill is located in the central region of Lunnan low bulge of Tabei uplift, Tarim basin. Ordovician Yingshan formation and Yijianfang formation are the major karst layers. The formation condition and the time of epigenic karstification of Lunnan ancient buried hill are very similar with Guilin karst in South China. With the study on the formation and distribution characteristics of epikarst in Lunnan ancient weathering crust and its influence factors, the following is gained in this paper. Epikarst belt, characterized by well developed karst fracture-cave system with certain connectivity, is range from 0 to 40m under the ancient weathering surface, which is the karst reservoir well developed part. The karst effective reservoir space is mainly corrosion pore, small-scale cave and corrosion fissure. The development of epikarst has close relationship with paleo-topography and paleo-hydrodynamic conditions. Under the different paleo-topography and paleo-hydrodynamic conditions, the thickness and karst shape of the epikarst, as well as scale and filling characteristics of karst fracture-cave system in the epikarst are different.
Research review and developmental trends of technology in karst reservoir exploration in China
WANG Yong, SHI Ze-jin, HONG Cheng-yun
2011, 30(3): 331-340.
Abstract:
Exploration of karst reservoir are getting progress in the recent20 years in the following aspects. (1)Combination of conventional geology methods, modern testing technology and geochemistry; (2)Good application effects with new logging technology such as FMI, XMAC, DSI and CMR; (3)A great number of new data processing and data interpretation technology which aim at raising resolution and improving the precision of karst reservoir prediction coming forth and being improved. Compared with other technology and method, geophysics method is the most hopeful area of breakthrough progress. There are still many problems need to be considered and resolved, such as how to improve the technology of seismic data acquisition and processing in order to reduce the cost, how to improve its quality and to increase its fidelity performance, how to comprehensively use logging date and seismic date, how to solve the lack of multidisciplinary talent and workgroup. Those are not only the problems that we must confront but also the developmental trends of technology in petroleum exploration.
Rare earth element contents in speleothem determined by two dissolution methods
ZHOU Hou-yun, TANG Jing, YUAN Dao-xian
2011, 30(3): 341-347. doi: 10.3969/j.issn.1001-4810.2011.03.017
Abstract:
Rare earth elements (REE) in stalagmite SJ3 collected from NE Sichuan in central China were determined by two dissolving methods, one by 2% HNO3 and the other by a mixture of HF and HNO3. The results indicate that although detrital materials are common in speleothems, a complete dissolution of the calcite powder from SJ3 by HF + HNO3 does not significantly enhance the REE concentrations obtained. This suggests that REEs in SJ3 are not contained in resistant silicate minerals which may not be derived from the overlying soil layer directly. The REEs in SJ3 may be released from the soil under chemical weathering, adsorbed on the surfaces of colloidal and particle materials in karst groundwater and incorporated into SJ3. The results indicated that REE in SJ3 can be released with diluted acids.
The seasonal variation of soil CO2 concentration in epikarst in the Panlong Cave, Guilin
LI Tao, CAO Jian-hua, ZHANG Mei-liang, HUANG Yan-mei, CHEN Jia-rui, YAN Yi-ping, LI Guang-chao, ZHU Xiao-yan
2011, 30(3): 348-353. doi: 10.3969/j.issn.1001-4810.2011.03.018
Abstract:
Taking the Panlong Cave karst experimental site in Guilin as a case, long-term survey on soil CO2 concentration variations at regular intervals is done in two sample plots depression bottom and slope. The result shows that:(1) The soil CO2 concentration varies seasonally obviously. In the summer (May to August), the soil CO2 concentration is two or three times higher than that in the other periods. And it is closely related with temperature, precipitation and biological activities; (2)The soil CO2 concentration at the depression bottom is higher than that on the slope, especially in the summer, the soil CO2 concentration at the depression bottom nearly 1000 mg/m2 higher than on the slope; (3)In the vertical profile, the soil CO2 concentration increases with depth in most cases, but the CO2 concentration both on the slope(-50 cm and -80 cm)or at the depression bottom(-80 cm and -100 cm)reduce with soil depth during the rainy season, which make the soil CO2 concentration to increase with the depth at the top and decrease at the bottom of the vertical profile.
A study on the color variety of speleothems Jinghua Cave in Benxi, Liaoning Province
QIN Ya, CHENG Xin-min, CHANG Jian-ping, LI Ze-feng
2011, 30(3): 354-358. doi: 10.3969/j.issn.1001-4810.2011.03.019
Abstract:
Jinghua Cave is developed in thick-bedded limestone of the Middle Ordovician Majiagou Formation in Benxi, Liaoning. Speleothems in the cave have many primary colors, such as white, yellow, red, blue and black. On the basis of research on the cave, X RF analysis and thin-section identification under the microscope have done. It is confirmed that the white color comes from pure CaCO3, blue and black from Cu, Sr, Mn and Zn components in the speleothems, yellow and red from some elements like Fe and Mn with different valence under different conditions.
The numerical simulation to the mineral dissolution-release law in the coal gangue
LIANG Bing, CHEN Nan, JIANG Li-guo
2011, 30(3): 359-362. doi: 10.3969/j.issn.1001-4810.2011.03.020
Abstract:
In order to better control the damage to environment by gangue, the mineral dissolution-release law of the coal gangue under different temperatures and CO2 partial pressure is researched. Hydro chemical simulation to the mineral dissolution-release law of the coal gangue under different temperatures and CO2 partial pressure is done in light of the software of PHREEQC developed by the United States Geological Survey. The results show that all of the coal gangue minerals solubility increases with temperature, however, with the increase of CO2 partial pressure the coal gangue minerals solubility gradually trend to decrease with the rise of temperature. Except for quartz, the solubility of all minerals in the coal gangue increases with the increase of CO2 partial pressure. The solubility of carbonate(calcite)increases rapidly in a nonlinear way with the increase of CO2 partial pressure, but other salts only increase slowly with CO2 partial pressure. In the coal gangue, the higher the concentration of the CO2 partical pressure in the solution, the higher the output of the gangue chemical components released. The higher the temperature, the higher the output of the chemical components released from the gangue under good air permeability.