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2009 Vol. 28, No. 3

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Hydrological responses to land-use changes in karst area— A case study in Houzhai river, Guizhou Province
MENG Hai-hua, WANG La-chun
2009, 28(3): 227-234. doi: 10.3969/j.issn.1001-4810.2009.03.001
Abstract:
Selecting Houzhai underground river basin as a study area, a sinkhole-based semi-distributed karst hydrologic model, which is based o the analysis of ecological environment features and karst water formation mechanism, was proposed and the impact of land-use and vegetation cover changes on the catchment runoff and the relationship between yield flow parameter and confluence flow parameter in Houzhai catchment, Guizhou province was discussed by means of field investigation, data collection and modern spatial technology as well as geography information system and remote sensing technology in this paper. It is proved that after the eco-construction other flow yield parameters change little except the maximum soil moisture storage, confluence flow parameter changed little too and get less than that before eco-construction basically. It is also proved that, under the constant rainfall, flow yield decrease and the runoff which is under the vegetation coverage becomes smaller at low water level and becomes larger at high water level after the eco-construction.
A practical use of 34S in the investigation of karst groundwater resource in North China
Zhang Jiang-hua, Liang Yong-ping, Wang Wei-tai, Han Xing-rui, Hou Guang-cai
2009, 28(3): 235-241. doi: 10.3969/j.issn.1001-4810.2009.03.002
Abstract:
In view of geo-chemical background, there are three major origins for sulfate form the karst water in most karst shallow circulation system in North China, whose aquifers is Ordovician carbonate rock: (1) dissolution of gypsum in the middle of Ordovician;(2) oxidation and dissolution of the pyrite in the overlying strata of coal measures, which recharge the karst groundwater; (3) sulfate from surface water that is directly related with top soil. Many tests indicate that the 34S value in groundwater changes greatly among different sulfate radical origins. Generally, the sulfate isotope from sulfate radical in the middle of Ordovician is heaviest in the three kinds of water with a δ34S value of 20‰~ 32‰.while,the sulfate isotope from the pyrite in coal measures is lightest with a δ34S value of -10‰~ 10‰, which is mostly less than 4‰. The sulfate isotope from surface water is between the two kinds of origins mentioned above with a δ34S value of 7‰~12‰. In light of the tracing significance features, the relations between recharge and discharge and the origins of some hydro-chemical elements in some spring systems are successfully interpreted, which give powerful proof for further understanding of the hydro-geological conditions.
Temporal-spatial variation of SO42- concentration of the drip water and its significance in the Shihua cave, Beijing
Ban Feng-mei, Pan Gen-xing, Cai Bing-gui, Zhu Jian, Tan Ming
2009, 28(3): 243-248. doi: 10.3969/j.issn.1001-4810.2009.03.003
Abstract:
As a crucial element in environmental geochemistry cycle, sulfur reflects the environmental change on both regional and global scales. In this study, sulfate radical concentration form 4 drip water points (PL1, PL2, SH, JG) in the Shihua cave have been monitored for three years, and those form the drip water point(BL) was monitored for two years. Drip discharges show three types of response to surface precipitation variations: rapid response, response with associated time-lag and stable (no response). The results show that: (1) SO42- concentration in rapid response drip water increases sharply during rain period, and has a exponential relationship with drip rate.; (2) in the drip water of lag response, SO42- concentration has no significant increase during rainfall, but they show a increasing trend during a long-term monitoring; (3) SO42- concentration at the stable drip site is low and has no obvious change during wet season. This means that the sharp increase of SO42- concentration may influence to some extent the pH value at the rapid response sites, which results in the declined calcium saturation index (SIc) of the drip water in rainy season. So it may be a indispensable factor to restrain the deposition rate of the drip waters in the Shihua cave.
Study on organic pollution of karst underground water in Jinan spring area
Xu Jian-guo, Zhu Heng-hua, Xu Hua, Liu Chun-hua, Zhang Zhuo
2009, 28(3): 249-254. doi: 10.3969/j.issn.1001-4810.2009.03.004
Abstract:
This paper carried out a systematic sampling and analysis on water quality of Jinan spring system .The results show that karst water in Jinan has generally been polluted by organic pollutants, which detection rate is up to 93%. The water samples with more than 5 items of organic detected are mainly found around the large and medium-sized enterprises. Among all the organisms detected, the organochlorine pesticide category and halohydrocarbon category get the highest detection rate as 60% and 57.8% respectively. Although organic pollution is widespread, the organic pollutants exist in karst water with a low content, and superscalar phenomenon only exists in local area. The organic pollutants distribution in spring area is controlled by industrial enterprises location and groundwater flow. The nearly rectangular shape of the karst water of organic pollution formed in southern margin of Jinan intrusive rock body, covering an area of 156km2. The southern contaminated area is the industrial zone, with shallowly buried limestone and poor anti-fouling properties. Besides, the groundwater flow direction and intrusive rock body in the southern edge meet nearly vertically with each other, so the organic pollutants can be transported toward north into the limestone aquifer with the groundwater, which leads to the karst groundwater lying under the igneous rock to be polluted.
Analysis on karst groundwater system and its water resources composition in Shiqihe basin
Lao Wen-ke, Lan Fu-ning, Jiang Zhong-cheng, Qin Xiao-qun, Xie Yuan-qiu, Deng Yan
2009, 28(3): 255-262. doi: 10.3969/j.issn.1001-4810.2009.03.005
Abstract:
Based on the further study on the aquifer structure characteristics and water resources formation of the karst groundwater system in Shiqihe basin, the flow attenuation process after the last flood peak in 2005(the biggest flood in the year) was taken as the data source to establish a total discharge-flow attenuation equation through the series analysis on the long-term observation data of the dynamic flow at the total discharge site. And then, the water resources composition was studied and analysis by means of the attenuation equation in the paper. The results show that total natural karst water discharge of the Shiqi river is 69 469.95×104 m3during the largest flood peak in 2005, which is composed of 4 parts: Slope runoff accounts for 3.64%, large scale karst conduit flow accounts for 4.53%, small karst conduit flow or strong developed karst fissure flow accounts for 74.10%, and small karst fissure flow accounts for 17.73 %. From the initial attenuation (can be regarded as the effective karst water resources), those flow can last for 2, 8 and 35 as well as more than 126 days respectively.
Analysis on hydro-chemical features and origin of the hot spring in karst geothermal field, east Liaocheng city
ZHANG Bao-jian, Shen Zhao-li, Qiao Zeng-bao, Qi Lin
2009, 28(3): 263-268. doi: 10.3969/j.issn.1001-4810.2009.03.006
Abstract:
Based on the analysis of chemical composition, isotopes and hydro-geologic features of the hot spring in karst geothermal field, east Liaocheng city, the origin and evolution of the hot spring were studied in the paper. The results show that the formation of the hot spring is controlled by deep faults and basement structure. And it is the consequence of natural comprehensive function during a long geological history. The hot spring is moderate or high degree metamorphic water originated from the infiltrating modern meteoric water, among which forty-year old ancient water dominates, while the new water is less, which can be explained by the relationship between δD and δ18O and tritium (T) values and coefficient of hydro-chemical characteristics. The formation of hydrochemistry ingredient is primarily leaching and dissolving, and the trace element ingredient is rich, which reflect that the groundwater passed through a long and complex runoff process and deep cycle.
Application of GIS to 1:50,000 karst hydro-geologic field survey— A case study in Xintian basin, Hunan province
ZHOU Li-xin, SHI Jian
2009, 28(3): 269-274. doi: 10.3969/j.issn.1001-4810.2009.03.007
Abstract:
Application of GIS techniques to karst hydro-geologic field survey usually spends a lot of time preparing digital data, which make GIS system can not be used in the fieldwork in time. In order to apply the GIS technique betimes on the fieldwork in the 1:50 000 composite hydro-geologic field survey ,the author edited and adjusted the digital data collected from Xintian basin by different methods based on the complexity of the data, and provided the fieldwork map that contained rich information in time, built the data platform for editing and analyzing in working area, input and analyze the data in time during the survey, edit the geologic borderline, check the position of the points recorded in field, find the miss information, optimize sampling route. All of the above has improved the data precision and work efficiency.
Application of ANSYS to early warning of soil cave evolution
QIN Xiu-ling, YAN Ming, Jiang Xiao-zhen
2009, 28(3): 275-280. doi: 10.3969/j.issn.1001-4810.2009.03.008
Abstract:
This paper took a highway in Guilin as a study case, chose TDR monitoring technology as a major research tools and used ANSYS to simulate the TDR to monitor the entire process, based on the comprehensive analysis on the existing early warning technology of the karst soil cave along highway covered area. The simulation results show that it may cause damage to ground surface if there is soil cave with a diameter of more than 3.0 m in the earth layer, which is 5.0 m or so away from the bed rock surface. If the layer thickness(5.0m) and beam cross-section size(8 cm × 6.5 cm) remains unchanged, ground deformation will be more obvious, and the deformation will presents as a slow linear trend, as the soil cave is growing upward slowly along the bed rock surface and its diameter keep on increasing. If the soil cave is 2.0 m long and 4.0 m deep, or it is 4.0 m long and 3.0 m deep, beam deformation tend to stability when it is buried at 2.0 m to 4.0 m depth. If the soil cave is 3.0 m long and 3.5 m deep, beam deformation are almost the same when it is buried at a depth of 1.0~3.0 m. If the soil cave is 5.0 m long and it’s roof is 2.5 m deep, beam deformation, which is 6.74 × 10-2 m and 6.75 × 10-2 m respectively, are basically the same when beam buried at 1.0m and 2.0m depth, which is also mean that it has reach the limiting equilibration.So it can more effectively monitor the soil deformation and the hole evolution trend that monitoring beams are laid within a depth of 2m from the roof of soil cave.
Professional evaluating system for karst tunnel gushing based on AHP and its application
DU Yu-chao, HAN Xing-rui, LI Zhao-lin
2009, 28(3): 281-287. doi: 10.3969/j.issn.1001-4810.2009.03.009
Abstract:
For the purpose of quantitative and semiquantitative description of impacting factors of the evaluating system for karst tunnel gushing, which will help us to predict the geological disasters directly and effectively, the paper has adopted Analytic Hierarchy Process (AHP) to quantitatively integrate multi-factors of tunnel gushing, with synthetic index (Skarst) for judging karst tunnel gushing being concluded, which will be used to evaluate the risk for tunnel gushing under different karst hydrogeological conditions. A case study of tunnel gushing by applying AHP has been operated in Wuchiba, and we have concluded the results as follows: the sections of ZK259+890~ZK258+500 and ZK255+405~ZK253+182 are the places with low risk for tunnel gushing, whose Skarst is lower than 0.24 (including 0.24); the sections of ZK256+300~ZK255+405 and ZK258+500~ZK257+500 are the places with middle-class risk for tunnel gushing, whose Skarst is in the range of 0.24~0.70(excluding 0.24, but including 0.70); the sections of ZK257+500~ZK256+300 is the place with high risk for tunnel gushing, whose Skarst is higher than 0.70 (excluding 0.70).
Study on lining external water pressure under limited discharge in deep buried tunnel
Wu li, Liu po-la
2009, 28(3): 288-292. doi: 10.3969/j.issn.1001-4810.2009.03.010
Abstract:
Lining external water pressure under limited discharge in deep buried tunnel is studied in the paper by means of theoretical derivation of tunnel discharge and lining water pressure model. It is proved that lining upper water pressure decreases along with the increase of discharge after adopting drainage measures, but the lining upper water pressure increases little with the increase of cementing scope when the permeability coefficient of grout drop below 1.65×10-6m/s and the grout thickness reach 55cm, which shows that there should be a reasonable scope for cementing. Grouting can control the discharge of tunnel. Grouting area can be defined when the reasonable discharge from a passage tunnel are given.
Study on the soil hydro-structure function of restored vegetations in the Yunnan Shilin park of China
ZhanG Yong, Wang Jing-jing, Li Yu-hui
2009, 28(3): 293-299. doi: 10.3969/j.issn.1001-4810.2009.03.011
Abstract:
Based on the requirement of ecosystem function assessment of restored vegetations in karst area, the soil hydro-structures function of restored vegetations were evaluated by the soil hydro-structure function model in the famous Shilin park in Yunnan province of China, which is a part of south China karst world natural heritage. Six vegetation sample plots, which form a succession of restored vegetations in the karst area ,including original forest (forest of Cyclobalanopsis glaucoides), 26 years secondary forest B (secondary forest of Cyclobalanopsis glaucoides), 21 years secondary forest A (secondary forest of Neolitsea homilantha) , 8 years brush, rock-desertification bushy grasses and 30 years secondary forest of Pinus yunanesnis, were chosen for assessment. As contrasted with the original forest, 31% of soil hydro-structure function can be restored after ecology recover and blockading administer for 8 years, and 45% can be restored after 21 years of ecology recovery in rocky desertification plots. And only 38% in secondary forest of Pinus yunnanensis can be restored after 30 years of ecology recovery, while 71% of soil hydro-structure function can recover after 26 years of eco-closing .The model of soil hydro-structure function is basically suitable for evaluation of restored vegetations in karst areas.
Evaluation on karst eco-environment sensitivity— A case study in Duyun city
LI Rong-biao, HONG Han-lie, YIN Ke, LI Yang-bing, YANG Guangbin, AN Yu-lun
2009, 28(3): 300-307. doi: 10.3969/j.issn.1001-4810.2009.03.012
Abstract:
Evaluation index system of eco-environment sensitivity was established in this paper, which is founded with six kinds of indexes, including stratum lithology, topographical slope, vegetation cover, land use and population density as well as average annual net income of farmers. Based on the 3S technology, the paper extracted evaluation indexes, built spatial analysis model for spatial overlay analysis of the evaluation indexes, and graded eco-environment sensitivity and its spatial distribution in karst area. Grade evaluation analysis was finally established according to the characteristics of spatial distribution. The results show that strong, moderate, light, minor and non-eco-environment sensitivity area cover an area of 75.23 km2, 228.32km2,902.11km2, 841.00km2and 231.35 km2 respectively, which account for 3.30%, 10.02%, 39.60%, 36.92%, and 10.16% of the total area of the whole city accordingly. At the same time,the research indicate that the problem of fragile eco-environment sensitivity in karst area is a result that the fragile eco-environment is disturbed perennial by human activities.
Effects of farming behaviors on soil quality in small karst basin
Liao Jing-Lin, Su Yue, Li Hang, Liu Fang, Feng Ze-Wei
2009, 28(3): 308-312. doi: 10.3969/j.issn.1001-4810.2009.03.013
Abstract:
Selecting Maodong small basin, Puding county, as a study area, we collected and analyzed the soil sample from different farming area influenced by different and long-trem farming method,which include dry-land in low multiple crop index,dry-land in high multiple crop index and composite-land in high multiple crop index.The results show,under the long-trem influence of different farming behaviors,the soil, collected from dry-land in low multiple crop index to dry-land in high multiple crop index to composite-land in high multiple crop index, decease in bult density, clay content,total P and activities of catalaes and increase in organic matter, humic acid contents, nitogen,available nitrogen, phosphorus, potassium, soi breathe intensity and urease, phosphatase, protease active content. C1uster analysis prove that preserving abi1ity of moisture and fertility and providing abi1ity of ferti1ity of the soil are best in high mu1tiple crop index but worst in low mu1tiple crop index. The above conc1usions show that the behavior of the farmer affects the soil quality to some extent。
Study on two quantitative methods of soil quality assessment in Huajiang karst canyon
ZHOU Wei, ZHOU Yun-chao
2009, 28(3): 313-318. doi: 10.3969/j.issn.1001-4810.2009.03.014
Abstract:
Five kinds of land uses are taken to elucidate the soil quality changes in Huajiang karst canyon, Guizhou province. The results show that the soil quality changes evidently under different land uses. The soil quality under different land uses was studied by means of the soil quality index(QI) and the soil deteroration index(DI) in the paper. Results from both methods show a similar trend of soil quality under different land use condition, that is Shrubs land> High-forest>Reforest land>Arable land >Grassland. In addition, correlative analysis of the two methods reveal that, there is a significant linear correlation between DI and QI, with a R2 value of 9.277. Both methods are efficient in the evaluation of the soil quality levels under diffetent land uses.
Comparison between biomass and water absorbing capacity of mosses on limestone and lateritic in Laowanchang Lateritic Gold Deposit
WANG Wen-yun, ZHANG Zhao-hui
2009, 28(3): 319-323. doi: 10.3969/j.issn.1001-4810.2009.03.015
Abstract:
Perennial and devastating mining make a mass of limestone exposed to the earth surface and the eco-environment degraded seriously on Laowanchang gold deposit. After analyzing the biomass and saturated water absorbing capacity of the dominant mosses which are collected from limestone and lateritic gold sites in Laowanchang gold deposit, we have come to the conclusion that, on limestone, Didymodon vinealis (Brid.) Zander, Timmiella diminuta (C.Muell.) P.C.Chen, Tortula yunnanensis P.C.Chen, Didymodon rigidulus Hedw.and Anomobryum gemmigerum Broth. are dominant mosses, with a biomass of 859, 364, 292, 228 and 215g/m2, respectively, and their saturated water absorbing capacity are up to 1 780, 9 170, 1 530, 2 980, 2 120 g/m2, respectively. On ateritic gold sites, Didymodon vinealis Com., Pogonatum neesii Dozy , Didymodon rigidulus Hedw., Microdus brasiliensis (Dub.) Thér. and Anomobryum gemmigerum Broth. are dominant mosses ,with a biomass of 854, 596, 333, 158, 134 g/m2, respectively, and their saturated water absorbing capacity are up to 3 070, 10 020, 1 440, 1 710, 4 130g/m2, respectively. These results show that Didymodon vinealis (Brid.) Zander which owns the largest biomass is the mian preducer on limestone and lateritic gold sites, and its saturated water absorbing capacity is very high too. According to the analysis, it is found that the saturated water absorbing capacity is related to the biomass significantly, which means that the mosses, having large biomass, are able to absorb large quantity of water. Especially, Didymodon vinealis are of important realistic significance to the desertification control in limestone areas and the soil and water conservation in this mine.
Preliminary study on diatom biodiversity and environment in Tianhetan dry cave, Guiyang
LIU Ming, WANG Qian, MA Jian-rong, ZHAN Jin-xing, YIN Wei-rong, ZHI Chong-yuan
2009, 28(3): 324-328. doi: 10.3969/j.issn.1001-4810.2009.03.016
Abstract:
In order to study the distribution and biodiversity of karst cave diatom, enrich and accumulate the basic theory date of diatom research, the authors conducted a field investigation in Tianhetan dry cave, Guiyang in December 2008. After identifying and analyzing in laboratory, 7 Genus and 27 species, including variation, were found in Tianhetan dry cave, among which 7 dominance species were included. The diatom quotient is zero, average dominance of biodiversity indexes of genus and species are 0.113 and 0.023, and Shannon—Wiener indexes are 2.60 and 4.43, respectively, evenness degrees of both genus and species are approximately 0.93, average cell density of diatom is 1 609.36 cell/cm2. The results also show that diatom biodiversity in Tianhetan dry cave is higher than in the river, lake (or reservoir) and ocean, but the diatom body in Tianhetan dry cave is smaller. There is a good correlation between diatom and kast cave environment, so make use of diatom as an indicator for the evaluation and monitoring of karst cave environment will be of important scientific research value, theoretical and actual significance.