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2008 Vol. 27, No. 1

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Water resource exploitation from big karst spring by flow narrowing-water pressure adjusting-water table raising -- A case in Pijiazhai spring, Luxi county, Yunnan
WANG Yu
2008, 27(1): 1-5. doi: 10.3969/j.issn.1001-4810.2008.01.001
Abstract:
Water resource and energy resource are in short supply at present, so it is valuable to exploit more hydropower from ascending spring. This paper is to offer an effective demonstration to the exploitation of karst ascending spring. The Pijiazhai big karst spring is an ascending spring of 1 072.75~1 957.5L/s in discharge. Its outflow point is at a flat karst valley bottom in the upper part of the Luxi karst basin. The outflow point and runoff way are lower in elevation than the fields and the villages. According to the particular hydrogeologic and engineering geologic conditions, the original engineer technique program by narrowing flow, adjusting water pressure and is designed for the exploitation of the spring. The engineer design takes benefits of favorable conditions such as the higher confining water table, the weak permeable karst zone at the lower reaches and the superjacent impermeable soil layer around the spring outflow point. The engineer made up of the seepage-proof grouting curtain and the flow narrowing, water pressure adjusting tank. The water level is adjusted by opening and closing the lock gate on the tank to realize raising the water table and transporting the water to higher elevated area, and as a result enabling the spring an artesian irrigation source. The demonstration engineer now has replaced the former 17 pumping stations and eliminated the water logging hazards at the area downstream Pijiazhai spring.
Classification of karst groundwater system and statistics of the main characteristic values in Southwest China karst mountain
PEI Jian-guo, LIANG Mao-zhen, CHEN Zhen
2008, 27(1): 6-10. doi: 10.3969/j.issn.1001-4810.2008.01.002
Abstract:
The groundwater system in karst region is the basic water system in Southwest of China karst mountain. The classification of karst groundwater system is a foundation for estimation and use of water resources there. According to the outcome condition of karst water, 3 620 karst groundwater systems are divided, including 1 179 subterranean streams, 1 152 karst spring systems, 562 concentrated drainage systems and 727 decentralization drainage systems. Being based upon the outcome condition of terrain in karst region, five types are divided: bare karst (2 324), bare-covered karst(108), covered karst(275), bare-buried karst (88). Except decentralization drainage karst water system, there are 26 karst groundwater systems with the catchments bigger than 1 000 km^2 in area. In subterranean stream systems, there are 1 049 systems with the catchments between 10 km^2and 500 km^2 in area that accounts to 88.97% of the total, 711 ones with the catchments smaller than 100 km^2 in area that accounts to 60. 3%0 of the total. In karst spring systems, there are 814 systems with the catchments smaller than 50 km^2 in area that accounts to 70.66% of the total. In concentrated drainage systems, there are 303 systems with the catchments between 100 km^2 and 500 km^2 in area that accounts to 53.91% of the total. The result of runoff statistics shows that 286 groundwater systems is more than 1 000 L/s in runoff that accounts for 11.2% of the total and 630 ones are between 50 L/s and 500 L/s in runoff that accounts for 63.73% of the total.
Analysis to gushing in Wuchiba tunnel and features of karstification
DU Yu-chao, LI Zhao-lin, HAN Xing-rui, LI Guang-hui
2008, 27(1): 11-18. doi: 10.3969/j.issn.1001-4810.2008.01.003
Abstract:
There are six types of karst physiognomy in Wuchiba and two karst water systems (with three underground rivers) relate to the tunnel. The Baiyanba subterranean stream is controlled by the types of carbonate rocks with simple conduit structure and featured hydrogeologically by being of lateral recharge and longitudinal discharge. The Longtang and Maotian subterranean streams are controlled by geologic structure and featured with multilevel conduit branch and discharge way. The Wuchiba highway tunnel is divided into three parts and five sections of karst zone by the author. Method of infiltration coefficient of precipitation, modulus method of groundwater runoff and analogy method of hydrogeology are adopted to calculate and forecast the rate of gushing water in each subsection. Then, the influence of karstification features in each subsection on gushing water is analyzed and concludes that the maximum rate of the tunnel attains to 31.3× 10^4m^3/d between ZK256+300 to ZK257+000 section.
Causes of spring's of flux attenuation and simulation of spring's regime --A case in Jinan karst spring area
WANG Mao-mei, SHU Long-cang, JI Ye-fei, TAO Yu-fei, DONG Gui-ming, LIU Li-hong
2008, 27(1): 19-23. doi: 10.3969/j.issn.1001-4810.2008.01.004
Abstract:
Take Jinan karstic spring as an example, the statistical method combined with the statistical software SPSS is used to analyze the regime of karst aquifer system. According to the 38 years' monitoring data, spring flow regime process was divided into two periods (1959-1968 & 1969-1996), and partial correlations analysis has been made in two different period. The result shows that natural factor is main factor in the previous period. However, natural factor and human activity are the main factor in the latter period. On the basis of partial correlation analysis, mathematical model of each period is developed and the spring flux is simulated and predicted. The error of simulation period is 2% and prediction period (1981-1987) is 3.4%. The fitting and prediction result is good.
Influences of SO42- on the solubility of calcite and dolomite
YAN Zhi-wei
2008, 27(1): 24-31. doi: 10.3969/j.issn.1001-4810.2008.01.005
Abstract:
A computer analogue is given to simulate the influences of SO4^2- ion on calcite and dolomite solubility in Na2SO4,CaSO4 and MgSO4 solutions with different Pco2 at 25℃ by means of the software for hydrogeochemical modeling -PHREEQC. The results show that the existence of SO4^2- ion in solution raises calcite and dolomite solubility considerably. For example, the solubility of the calcite and dolomite in Na2SO4 solution with 1 200mmol/L in concentration and Pco2= 0 at 25 ℃ are 9. 544 and 9. 897 times greater respectively than those in pure water. The chemical mechanism for this is as follows: when common ions do not exist in solution, salt effect and ion pairs raise the solubility significantly. As common ions exist in solution, incongruent dissolution will take place, thus helps dolomitization or dedolomitization to occur. It is also concluded that the salt effect in all the cases should not be neglected including even in the cases with common ion especially when SO4^2- concentration is high.
Impact on the Daning river sedimental environment by Three Gorge Reservoir in view of changes in sediment compositions
WANG Yong, LI Hong-chun, LUO Shang-de, GUO Fang-xu, CAI Jin-lang, WANG Jin
2008, 27(1): 32-37. doi: 10.3969/j.issn.1001-4810.2008.01.006
Abstract:
This study shows the results of analysis to X-ray diffraction (XRD), total carbon (TC) and the total organic carbon (TOC) contents of fluvial sediment core nearly 42cm long collected from the Daning river. Three primary results are concluded: (1) The XRD results indicate that quartz and calcite are the dominant minerals in the sediment. The TC and TOC contents range from 33 to 57g/kg and from 8 to 34g/kg, respectively. (2) From 10cm deep toward the core top both TC and TOC continuously decrease and the sediment become brown color. The Three Gorge Reservoir may elevate water level and leads to dramatic increase in input of brownish low carbon content clay sediment into the Daning river. Then the sediment rate of the Daning river will be increased dramatically by this mechanism. (3) From 10 to 17 cm deep in Shuanglong profile, TOC content in the sediment dramatic increase may be resulted from intensive human activities which lead more organic matter input into the Daning river..[
Preliminary study on pH abnormality and the causes in inland high-mountain gorge -- A case in Shuzhenggou and Rizegou, Jiuzaigou area
YUAN Hong, YUAN Dao-xian, FU Wa-li, WANG Gai-gai, ZHANG Zhi-wei
2008, 27(1): 38-42. doi: 10.3969/j.issn.1001-4810.2008.01.007
Abstract:
The soil acidity is the foundation that we study other physical and chemical properties of soil. At present, because of environmental pollution and acid rain, the soil is going to be acidified in most karst areas. But by sampling analysis, it is found that karst swamp soil acidity in Sichuan Jiuzaigou is between 7.72 and 9.10, and this is high to other kind of karst soil. The biggest discrepancy reaches to 4.85 units. Among 26 sampling spots, there are 17 spots with pH value exceeds 8.00, about 65% of the total. There may be four reasons for this : geological and deep layer circle ; conversion process of soil organic materials ; the action of soil colloids and deposition of a great quantity of travertines. It is also put forward in this paper that all factors should be further studied by means of modern method such as steady carbon and oxygen isotope, local chemical exploration to hydro-deposition. All the above efforts are guarantees to sustainable exploitation and utilization as well as protection to Jiuzhaigou.
Study on the geochemical properties of Fe-Mn nodule in Litang karst area
SU Chun-tian, TANG Jian-sheng, SHAN Hai-ping, CHEN Hong-feng, XIA Ri-yuan, ZOU Sheng-zhang
2008, 27(1): 43-49. doi: 10.3969/j.issn.1001-4810.2008.01.008
Abstract:
In this paper, the geochemistry properties of Fe-Mn nodule are studied in Litang karst area. Compared with corresponding soils, SiOz, Al2O3 and Fe2O3 are still the main elements in the Fe-Mn nodule. However, the Fe2O3 content increases significantly and is the most in the oxides, meanwhile the MnO content increases to some extent with the enrichment coefficients being 5.19 and 3. 40. The Fe-Mn nodule enriches heavy metal elements, the enrichment order of some heavy metals is Cr( Ⅵ )〉Pb〉Co〉Zn〉Ni〉Ba〉 Li. The Fe-Mn content in the soil is affected by parent rock of the soil and shallow groundwater. By correlation matrix analysis and factor analysis, it is proved that there are the nucleation and enrichment effect, the specific adsorption effect and the leaching effect.
Comprehensive improving technique to rocky desertification in karst peak-cluster depression -A case study at Guohua Ecological Experimental Area,Pingguo, Guangxi
JIANG Zhong-cheng, LI Xian-kun, QIN Xiao-qun, LU Shi-hong, LUO Wei-qun, LAN Fu-ning, CAO Jian-hua
2008, 27(1): 50-55. doi: 10.3969/j.issn.1001-4810.2008.01.009
Abstract:
With typical karst peak-cluster depression landform,poor people and heavy rocky desertification, Guohua Ecological Experimental Area in Pingguo county, Guangxi is about 600 hm^2. Since 2001, the Eco- logical Experimental Area has been built. After investigation and researches to the environments and regional economics in detail, the stereo eco-agricuhure in different geomorphologic position of the peak-cluster depression is considered as an available model for the comprehensive improvement to rocky desertification. Meanwhile, a lot of related technique and methods for the improvement of environments and the development of agriculture are imported, studied and put into practice, such as forestation of 310 hm^2 hills, exploitation of more than 10 000 m^3/a karst water resource, development of ecological industry, planting of grassland for breeding of domestic animals, and improvement of karst soils. For about four years, the comprehensive improvement of rocky desertification in the experimental area has achieved good results. The vegetation is grad- ually restored, the annual mean income of the local people has increased by about 20%, and the new local ecological industry is formed.
Studies on the regime of soil moisture under different microhabitats in Huajiang karst valley
LI An-ding, LU Yong-fei, WEI Xiao-li, YU Li-fei
2008, 27(1): 56-62. doi: 10.3969/j.issn.1001-4810.2008.01.010
Abstract:
Soil physical characters and soil moisture regime law under different microhabitats on afforestation land in karst stony hill area of the Huajing river valley are studied. The result shows that water condition of stone gully is best and soil surface is between stone gully and stone pit, but stone pit is worst. The time of high moisture condition period and that of low moisture condition period under different microhabitats obviously changes annually. Times, extent and dates of water stress under different microhabitats is also actually different in one year. Loss of soil moisture is fast in stone pit, but slow on soil surface, and in stone gully it is between stone pit and soil surface at three small sites within continuous drought dates, which is separately 17.30%, 14.49% and 13.87% in seven days. Time of slight stress on soil surface, in stone pit emerged in seven days. Therefore, soil water stress under different microhabitats emerged in Huajiang karst valley in seven days. This data may be regarded as the time for supplement of water to plants. In general, soil moisture condition in stone gully is superior to soil surface and stone pit. Directing at soil moisture regime character under different microhabitats, suggestion for choosing and allocating tree spices and management to soil water is put forth in the paper.
Soil microbial activities during regeneration of the degraded karst vegetation -- A case study at Huajiang, Guizhou
WEI Yuan, YU Li-fei, ZHANG Jin-chi
2008, 27(1): 63-67. doi: 10.3969/j.issn.1001-4810.2008.01.011
Abstract:
The regeneration mechanism of the degraded karst vegetation has been the research focus of soil science and ecology in China for the last decade. The amount of soil microbes, soil biochemical function and soil microbial biomass are analyzed during restoration of the degraded karst vegetation and the change of soil microbial activities was studied on ecological synthesis control demonstrated area in Huajiang karst plateau, Guizhou. The results showed that,with degraded karst vegetation restoration, the amount of bacteria, fungi, antinomies and total microbial amount ascend obviously, performing bare land stag〉herbaceous community stag 〉shrubby community stag 〉 arboreal community stag. Compared with the fungi and antinomies, the bacterium is dominant and the proportion is 95. 95%, 93. 49%, 92. 32% and 92. 48% in microbial amount. The amount of major physiological group are increasing, ammoniating bacteria〉nitrifying bacteria 〉cellulose decomposing microbes〉 nitrogen-fixing bacteria. Soil biochemical function, including ammonification, nitrification, cellulose decomposition, respiration and nitrogen fixation are increasing. The soil microbial biomass C ascended significantly. There is a significant positive relationship between soil microbial biomass C and organic C (P〈0.01). Soil microbes are recommended as one of major characteristics of soil quality during degraded karst vegetation restoration. It reflects that soil quality is restoring gradually with degraded karst vegetation succession.
Quantitative study on land cover changes and the driving forces in Maotiaohe basin
PENG Jian, XU Yue-qing, CAI Yun-long, WANG Le
2008, 27(1): 68-74. doi: 10.3969/j.issn.1001-4810.2008.01.012
Abstract:
In recent years, Chinese scholars have focused more on the karst rocky desertification issues in Southwest China. However, the comprehensive research on land use and land cover change in this area, which is closely related to the karst rocky desertification problem, has been paid little attention. By using the integrated technique of RS, GIS and GPS and by employing the methodology of Canonical Correlation Analysis, the authors have quantitatively studied the land use and land cover change processes and also their driving forces over the past 30 years. The results reveal that the area of arable land, construction land, forest land, water area, and rock-exposed land increased from 1973 to 1990 while grassland and shrub land reduced, which means that the eco-environment deteriorated in general. After 1990, forest land, grassland, construction land, and water area had kept increasing while grassland changed a little and arable land and rock-exposed land reduced, which suggests that the coo-environment tends to become better in Maotiaohe basin. Moreover, the quantitative research shows that it was the factor of total population amount that drove the change of construction land in the study area before 1990, but the factor of gross agricultural product after 1990. The increase of agricultural population was mainly responsible for the change of arable land before 1990, but the increase of corn yield after 1990.
Ecologic capacity analysis and sustainability estimation to ecological vulnerable karst region in Southwest Guangxi -- A case in Pingguo county
XIANG Wu-sheng, LI Xian-kun, HE Cheng-xin, LU Shu-hua, LU Shi-hong
2008, 27(1): 75-79. doi: 10.3969/j.issn.1001-4810.2008.01.013
Abstract:
Ecologic footprint is an effective way to measure regional ecologic capacity and sustainability. Taking the representative karst ecologic vulnerable region, Pingguo county, as an example, the regional ecological footprint and ecologic capacity are calculated by means of the statistic data in 1990, 1995, 2000 and 2002. And then, on the basis of the results, the sustainability of regional ecosystem is analyzed. The results show that, from 1990 to 2002, the regional ecologic footprint increased continuously from 0. 8004 hkm^2/per cap to 1. 4444 hkm^2/per cap. The ecological capacity also increased by 26.83% from 1990 to 2002, but the value was very small in comparison to the average level in both Guangxi and China during the corresponding period. On the contrary, the ecologic capacity of arable area and pasture represent a decrease trend. Except forest and garden land, ecologic deficit has occurred in arable area, pasture and water area. Overall, the regional ecologic balance between ecologic capacity and ecologic footprint show increasing ecologic deficit, which indicates that the regional development is unsustainable.
Evaluation model of ecotourism in Southwest China karst region
YAO Chang-hong, CHEN Tian, LIU Jia-ming
2008, 27(1): 80-85. doi: 10.3969/j.issn.1001-4810.2008.01.014
Abstract:
Southwest China karst area is one of the main karst zones in China and also the tour focus in the world. Because of the unique karst landscape and the virgin environment the ecotourism has developed rapidly there in the past 20 years. But lots of environmental challenges aroused and the development decelerated heavily for its special karst environment and environmental vulnerability. Therefore, the karst ecotourism theoretical system is advanced based on former theories and an evaluation model named PRIM model is founded. The PRIM model is made up of 4 parameters (Pollution, Risk, Interaction and Monopolization), 12 factors and 5 modified indexes. By discussing six tourism elements with PRIM model, the development model to karst ecotourism is brought forward for social/ environmental/ economic efficiency and fit for Southwest China karst region. The ecotourism situation of evaluated object can be indicated by value of Et which is the result of the PRIM model. By the way, primal problems and perfect measures can be brought out by the value of 4 parameters (Pollution, Risk, Interaction and Monopolization). The PRIM model was applied to evaluate the ecotourism situation of Lunan Stone Forest, Lijiang river and Tian'edong cave. By the results, Lunan Stone Forest and Lijiang River are normative ecotourism and the value of monopolization parameters is high, but Tian'edong cave proximate ecotourism and the risk and monopolization parameters are sensitive. The PRIM model is the first mathematical model to evaluate ecotourism in vulnerable karst area, and it is an attempt to set up a mathematical model to develop ecotourism theories. The study is beneficial to karst ecotourism development and the frontier of tourism knowledge.
Karst cultural tourism resources and their exploitation - A case study in Guizhou province
DU Fang-juan, XIONG Kang-ning, GAO Hong-yan
2008, 27(1): 86-90. doi: 10.3969/j.issn.1001-4810.2008.01.015
Abstract:
Karst environment has bred the unique karst culture. There is abundant and unique karst cultural tourism resources in karst area, such as farming, settlement,building, burial in caves,the folk custom and the household ware,are all stamped with the brand of "karst". The resources take pride in the scientific value according to local conditions ,the abundant historical and cultural information ,the culture value with the style that they are mixed but significantly different from each other,and the highest aesthetic value reflected in the harmony between human and nature. So the author takes Guizhou province as an example,and thinks the exploitation and utilization of tourism resources should abide by the general guideline of "karst culture" in karst area. Then, dig its connotation combining time and space when we design the tourist products..[
Inspection analysis of environmental change of karst cave -- A case of Jiutian cave in Yiyuan county, Shandong province
WANG Xiao-qing, ZHOU Chang-chun, SUN Xiao-yin, WU Chuan-zhen
2008, 27(1): 91-96. doi: 10.3969/j.issn.1001-4810.2008.01.016
Abstract:
In order to improve the cave's environmental quality and provide scientific basis for the protection of cave landscape, two times monitor on the spot from 1 to 5, May and 28 to 30, July, 2006 have been taken to monitoring the regime of temperature and humidity as well CO2 concentration of the Jiutian cave with the number of tourists. It is proved that the CO2 concentration is affected by the number of tourists and is of obvious accumulative effect. Among the monitoring spots, No. 11 (Lingxiaoyu Tower) has the highest average daily CO2 concentration with the value 11 250 ppm that is very rare all over the world. The temperature of the cave is affected both by cave drip water and by the shapes of the cave, and changes to some extent. Humidity of the cave is affected by the weather but also by respiration of the tourists especially in the enclosed sections of the cave.