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2010 Vol. 29, No. 2

Display Method:
Experiment and significance of rocky desertification harness in geological methods in Jumu Underground River, Guizhou
WANG Ming-zhang
2010, 29(2): 107-112. doi: 10.3969/j.issn.1001-4810.2010.02.001
Abstract:
The rocky desertification harness in Jumu Underground River is an experiment in light of geoscience. The goal of the experiment is to improve the karst geologic environment in rocky desert. By means of underground river exploration and mineral element fertilizer applying compensation during the growth season of crops, security of drinking water for people and livestock as well as irrigation is resolved; output and quality of crops is increased; local economy developed significantly and the unreasonable human engineering is controlled effectively. Remote sensing monitoring results show that the area of rocky desert has decreased obviously and that the extent of desertification has reduced remarkably after the experiment, which proves that to improve geologic eco environment is one of the efficient paths to harness rocky desertification and worthwhile to promote and popularize. However, the karst system in southwest China is very complicated and varied with comparatively great difference among different karst systems, therefore more effective harness should base on synthetic harnessing program according to practical geologic conditions.
Aalynological assemblage characters and the ecologic significanceamong rocky desert of different grades — A case in Huajiang
ZHAO Zeng-you, YUAN Dao-xian, LUO Lun-de, SHI Sheng-qiang, HAO Xiu-dong
2010, 29(2): 113-119. doi: 10.3969/j.issn.1001-4810.2010.02.002
Abstract:
Taken the demonstration plot in the Beipangjiang basin to the south Guangling County, Guizhou Province as an example, the authors analysis palynological assemblage characters from surface soil among rocky desert of different grades, reveal the relations between n palynologyical assemblage characters and rocky desertification grades. The results show that the palynological assemblage characters is of distinct individuality in rock desert with 16.1% of arbor and shrub and 58.9% of herb and fern, which reflects herb and fern are the dominate plants in the vegetation of rock desert. The results also show that the palynological assemblage quite correlates to the grades of rocky desert, i.e. the content of herb and fern goes up from 41% to 77.6% wit h the species from 14 up to 27, but the content of arbor goes down from 6.9% to 2.6% without species changes along with the increases of the grades of rocky desert. The palynological assemblage characters reflect that ferns like Pteris trifur cata Ching can adapt the desert environment and has representativeness in these regions.
The mechanism of underground leakage of soil in karst rocky desertification areas—A case in Chenqi small watershed, Puding, Guizhou Province
TANG Yi-qun1, ZHANG Xiao-hui, ZHOU Jie, SHE Tian-yu, YANG Ping, WANG Jian-xiu
2010, 29(2): 121-127. doi: 10.3969/j.issn.1001-4810.2010.02.003
Abstract:
The underground leakage of soil is a special type of soil and water erosion in karst rocky desertification areas. Based on a case study in the Chenqi small watershed — a serious karst rocky desertification area, the process and mechanism of underground leakage of soil is illustrated. The results show that special geologic and environmental conditions in the karst area provide favorable transport channel and accommodation space for underground leakage of soil. Substantial leakage of surface precipitation is the force f or soil leakage toward underground. The disintegration of the aggregate into the finer particles makes the soil leak easier to move along the soil pores and the rock fissures and goes down into underground. In conditions of the infiltrating and softening by the water, the soils that deposited in the karst fissures or caves become more plastic and are able t o creep along the soilrock interface and migrate to the underground river which leads to the leakage of the surface soil. This study is expected to provide a theoretical support for the soil and water conservation in karst rocky desertification areas.
Actuality and countermeasures of the edatope problem in karst mining derelict land in Guizhou Province
ZHANG Yi-xiu, WANG Ji, ZHANG Hao
2010, 29(2): 128-133. doi: 10.3969/j.issn.1001-4810.2010.02.004
Abstract:
According to the analysis on the distribution and development as well as using status of the karst mining derelict land in Guizhou Province, it is found that there are four edatope problems: (1) serious heavy metal pollution, such as the Zn content gets up to 162.23~877.88 mg/kg, Pb 37.24~305.56 mg/kg and Cd 0.50~16.43 mg/kg in Hezhang and some other regions, which have significantly surpass the local background level; (2)drought habitat; (3)intensifying soil loss, with average erosion modulus up to 5 000~15 000 t/km 2.a in most case according to the investigation; (4)low biodiversity. The actuality of the rehabilitation and reclaimation to the derelict land is also introduced in the paper. Furthermore, the key problems and related technique needed to be studied for the harness of edatope problem in karst mining derelict land in Guizhou, such as amelioration for soil, synthetic botanic and microbial harnessing methods, recycling techniques etc. are put forth.
Study on land suitability for Hyloccreus undatus and some other plantsin karst area based on DEM-GRA
WANG Lei, HU Bao-qing, ZHOU You-you, HOU Man-fu
2010, 29(2): 134-140. doi: 10.3969/j.issn.1001-4810.2010.02.005
Abstract:
In light of adjust measures to local conditions, DEM is established based on GIS platform and land suitability for Hyloccreus undatus at 6 sample plots in Rengtun karst depression, Tiandeng County is analyzed comprehensively by means of GRA in the paper. The results prove that plot 2, 4 and 6 being gentler in gradient an d smaller in hill shadow as well as thicker in soil layer are quite suitable for Hyloccreus undatus; but plot 3 being thinner in soil layer and larger in hill shadow is not suitable for Hyloccreus undatus; plot 1 with higher gradient and other suitable conditions and plot 5 being laugher in hill shadow but suitable in other conditions are both suitable for Hylocereus undatus, which situated between the former two types. Among plot 2, 4 and 6, plot 2 is better correlated to the suitable conditions for Hyloccreus undatus and most suitable for Hyloccreus undatus growth. According to the above evaluations, the land suitability evaluation method is used in harnessing karst rock desert, and artificial replanting at suitable patches in Tuanle and Dushan as well as Xiaoshan karst basins is done with the survival rate of the replanted plants higher than 85% and grows well meanwhile.
Assessment on ecosystem fragility of karst mountain areas based on synthetic method— A case study in Puding Country, Guizhou Province
SHU Long-cang, KE Ting-ting, LIU Li-hong, ZHANG Rong-rong, LU Cheng-peng
2010, 29(2): 141-144. doi: 10.3969/j.issn.1001-4810.2010.02.006
Abstract:
Based on principle component analysis and taken 13 villages in Puding Country, Guizhou Province as the example, the authors analyze 9 variables influencing ecologic al frangibility, and calculate the fragility with Euclidean distance formula. The results show that the cultivated area is the most import ant factor in determining the ecological vulnerable degree and its weighted value is up to 0.189, and the average gradient is the second factor. Among the 13 villages, there are 7 villages falling into severely or extremely fragile areas. Especially in Pianpo village whose vulnerable degree is maximum both in potential fragility and stress fragility. The study area evaluated as a whole is classified as severely fragile areas with an ecological fragile degree of 0.653. According to the standard of estimation grade, the authors find the Puding Country belongs to moderately fragile degree and we must take measures to recovery the ecoenvironment by controlling the land use for agricultural.
Evaluation on ecologic safety of Chongqing
WEI Xing-ping
2010, 29(2): 145-151. doi: 10.3969/j.issn.1001-4810.2010.02.007
Abstract:
With the development of economic construction, people have higher requirements to the living ecoenvironment. Taken Chongqing as the example, 17 indicators are built based on the pressure state response conceptual model. Ecological security dynamic assessment and ecological safety spatial assessment in Chongqing are analyzed with the fuzzy membership degree method. The results show that the ecological security value in Chongqing is 2.384 and 2.114 in 1997 and 2002, belonging to insecurity state, and 1.704 in 2007, belonging to critically safe. The ecological security in Chongqing in 2007 distribute as follow: there are 13 districts in more secure area(1.0≤B*<1.5)in west Chongqing, which attains 1.414 2×104 km2 and accounts for 17.16% of the total area; 11 districts in critical security zone(1.5≤B*<2.0)in northwest Chongqing, which attains 1.539 3×104 km2 and accounts for 18.68% of the total area; there are 12 districts in unsafe areas in southeast and northeast as well as the middle areas of Chongqing, which attains 3.952 3×104 km2 and accounts for 47.96% of the total area; and that there are 4 districts in very unsafe area in northeast and southeast Chongqing, which attains 1.334 5×104 km2 and accounts for 16.20% of the total area.
Value evaluation on the eco-services function of Zanthoxylum planispinum var. dingtanensi woods in Huajiang Karst Valley
LI Wei-jie, WANG Ting-mei, WANG Gui-ping, CHEN Xun
2010, 29(2): 152-154,161. doi: 10.3969/j.issn.1001-4810.2010.02.008
Abstract:
In this paper, the eco-services function of Zanthoxylum planispinum var. dingtanensi woods in Huajiang Karst Valley are studied by means of interrelate d theory and methods. The results indicate that the total annual services value of Zanthoxylum planispinum var. dingtanensi woods in Huajiang Karst Valley is up to 96.9 billion yuan RMB, including 14.1 billion yuan RMB direct value and 82.8 billion yuan RMB indirect values, indirect values is 5.87 times more than direct values. In the three indirect service items, the order of indirect value is below: soil and nutrient conservation >C fixation and O2 release >water storage , the evaluation date shows that Zanthoxylum planispinum var. dingtanensi woods eco system plays a significant role in the environment protection in Huajiang karst valley.
Study on the dynamic change of eco-footprints in Guizhou karst areas
YANG Ting-feng
2010, 29(2): 155-161. doi: 10.3969/j.issn.1001-4810.2010.02.009
Abstract:
In order to quantitatively discover the human social and economic activity effecting the dynamic change of natural environment in Guizhou karst area, the regime and structural conditions of the eco-footprints are analyzed by means of quantitative research methods of eco-footprints model according to history data from 1978 to 2008. The results show that per capita eco-footprints in Guizhou Province is on the increase in the research period and exceed the national average from 1997. And the long-time average annual major consumption focuses in three kinds of footprints: fossil fuel land and farmland as well as grassland. The eco-footprints for each 10,000 Yuan of GDP keep decreasing from 1978 to 2008, but the average for many years is still 2.3 times higher than the national average. In light of the above account,6 related regulative countermeasures are put forward, 1) enhance the efficiency of the existing resources and establish perfect management system; 2) positively use advanced technology and enhance natural system productivity; 3) govern an d restore karst ecosystem and protect agroecosystem; 4) control population quantity and improve the population quality; 5) develop hydro energy and low carbon economy, save energy and adjust energy structure; 6) actively enlarge regional contact and cooperation to promote trade with other regions.
Study on bryophytes in dolomite type mercury mine of Muyouchang in Guizhou, China
CHEN Xiao-peng, WANG Zhi-hui, ZHANG Zhao-hui
2010, 29(2): 162-169. doi: 10.3969/j.issn.1001-4810.2010.02.010
Abstract:
Bryoflores, collected from 6 habitats in dolomite type of Muyouchang Mercury Mine in Guizhou, China is analyzed in the paper. The results prove that (1) the bryophytes in dolomite type of Muyouchang Mercury Mine consists of 85 species, 37 genera, 12 families and the dominate families include Pottiaceae, Bryaceae and Brachytheciaceae. The bryophytes which belong to the three families are fit to g row in dolomite type of Muyouchang Mercury Mine; (2) Pottiaceae, Bryaceae and Br achytheciaceae distribute 4 common habitates which are mullock, waste residue, mine hole and stream. Furthermore, Pottiaceae and Bryaceae grow on waste furnace while Bryaceae and Brachytheciaceae belong to epiphyte; (3) the species similarity coefficients of waste furnace and waste residue, waste residue and stream, waste furnace and stream, waste residue and mine hole, mine hole and stream, waste furnace and mine hole on which bryophytes grow are 0.49, 0.46, 0.45, 0.41, 0.35 and 0.31 respectively which shows that the relationships are proximity. The species similarity coefficients between the bryophytes in mine hole and epiphytic b ryophytes and between epiphytic bryophytes and the bryophytes in stream are 0, which shows that the relationships are not exist; (4) the phytogeographical elements of the bryoflora include North Temperate(27.06%), Endemic to China(24.71%), E astern Asia(17.65%), Tropical Asia(14.12%), Cosmopolitan(7.06%), Pantropical(3.53%), Old World Temperature(2.35%), Tropical Asia and Tropical Australia(1.18%), Tropical Asia and Tropical Africa(1.18%) and Temperate Asia(1.18%); (5) the life forms are short turfs(71.76%), wefts(21.18%), tall turfs(2.35%) and mats(2.35%) as well as annuals(2.35%).
Comprehensive evaluation on carrying capacity of water resources based on the artificial neural network — A case study in Guizhou Province
ZHENG Chang-tong, LIANG Hong
2010, 29(2): 170-175. doi: 10.3969/j.issn.1001-4810.2010.02.011
Abstract:
This paper uses BP network to evaluate the water resource carrying capacity in karst area and compares the evaluating results with that calculated by gray relational projection method. Evaluating results of the two methods are similar overall. However, the water resource carrying capacity in Anshun and Tongren calculate d by the two ways is quite different. The result of BP network shows that the water resource carrying capacity in Tongren is the greatest, while Anshun is very small, only higher than Guiyang. But the result of gray relational projection shows that the water resource carrying capacity in Tongren is much lower than that in Anshun. To compare with former research results, it is proves that the method of BP network is more reasonable. By means of Kohonen network, the analyzed results show t hat the amount of water resources and economic level is the dominant factors impacting the water resource carrying capacity. In addition, the population has a greater influence to the water resource carrying capacity in Zunyi. The influence of karst conditions to the water resource carrying capacity in Tongren and Bijie is higher than other regions.
Appraisal of the karst development features and engineering geology conditions at a building site in Dayaowan, Liaoning Province
GUO Chang-bao, GUO Shu-tai, PENG Tao, LI Yao-gang, CUI Xue-tao, GUO Yin, WANG Shu-dong
2010, 29(2): 176-182. doi: 10.3969/j.issn.1001-4810.2010.02.012
Abstract:
The major bedrocks in Dayaowan are moderate to strong soluble carbonate rock with well developed fissure, so karst is strongly developed under the impact of sea water and groundwater as well as karst fissure water. The surveying drilling proves that the karst cavity discovering rate is 70.27%. The cavities mainly distribute between 20~30 m underground, and between 30~40 m secondly. The karst cavities are divided into 4 classes according to their size (h) in this article: the large scale (h≥4 m), the medium to large scale (2 m≤h<4 m), the medium (0.5 m≤h <2 m) and the small (h<0.5 m). The statistic result indicates that karst cavities in the location are mainly the medium ones, and secondly are the small or the medium to large scale ones. The growth and distribution of the karst cavities seriously affect the engineering geology conditions of the building site. Regarding the karsts as the major engineering geology problem, the background and forming conditions as well as distribution of karst at the building site are analyzed and e valuated in the paper. Accordingly, it is believed that the groundwork of the building site is karst laterite with moderately or strongly developed karst and the CFG and Vibratory Crushed stone composite piled foundation or some appropriate piled foundation etc. should be adopted in disposal this kind of groundwork in order to keep the engineer safe.
Preliminary study on risk assessment of water and mud inrush in karst tunnel
MAO Bang-yan, XU Mo, JIANG Liang-wen
2010, 29(2): 183-189. doi: 10.3969/j.issn.1001-4810.2010.02.013
Abstract:
Through analysis of more than 20 karst tunnels a risk classification system for water and mud inrush is put forth by means of qualitative and quantitative analysis on the condition that fully considering the operability and applicability of the methods used in the analysis. The 1st order evaluation index involves the material components of the soluble rocks and geotectonic conditions as well as field effect conditions; the 2nd order evaluation index involves 13 influencing factors such as the width of the faults and pressure of the confined water and the landform as well as the buried depth of the tunnel. In addition, the weights are determined with ATP and the degree of membership by means of qualitative and quantitative method, and the corresponding protect measures is drafted in light of the risk of water or mud inrush in the tunnel. The results show that the very risky part of water or mud inrush in Maoba syncline is 992 m long that accounting for 54.7% of the total tunnel.
Origin of ground collapse at the Sujiazhuang iron mine in Jinan City
WANG Qing-bing, GAO Zong-jun, DUAN xiu-ming, WU Li-li
2010, 29(2): 191-195. doi: 10.3969/j.issn.1001-4810.2010.02.014
Abstract:
Based on the survey to geologic conditions and exploitation situations at the Sujiazhuang iron mine,the features and origin of ground collapse is expounded by means of the analysis on geophysical features, sinking and driving engineering, groundwater table and engineering geologic features of the ore body an d surrounding rocks. The results show that the horizontal change of apparent resistivity isoline is relatively gentle within the 200 m probe scope with transient electromagnetic method and that there is no obviously abnormal distribution of goaf; the total volume of goaf is only about 9 218 m3 that is much smaller than the total volume, 58 665.8m3, of the collapse pit; the water head between the shaft and collapse pit and that between the collapse pit and goaf are very high and stable, up to 58.93~64.11 m; the integrity and intensity of the surrounding diorite and limestone as well as marble are quite well, so the probability of ground collapse led by goaf collapse is very small. According to the above situation and the comprehensive analysis on the landform, stratum structure, overlying cap, dynamic conditions and mine drainage as well as other factors, it is believed that the ground collapse is caused by long term pumping during exploitation.
Preliminary study on morphology features of karst in the lower reaches of Wujiang River — A case in Wulong, Chongqing and the surrounding area
XIA Kai-sheng, YUAN Dao-xian, XIE Shi-you, CHU Yu-chun
2010, 29(2): 196-204. doi: 10.3969/j.issn.1001-4810.2010.02.015
Abstract:
The geomorphology is typical subtropical karst Middle Mountain and gorge with characteristics of large scale karst gorge, natural briddge, tiankang, cave and underground river as well as colorful second deposits at the lower reaches of the Wujiang River. The karst individual feature and feature complex on stratified relief plane are analyzed and the evolution of the karst morphology at the lower reaches of the Wujiang River is studied in the paper. It is believed that 1) the stratified relief plane can be divided into 2 grade planation surfaces, 1 grade corrosion surface, 5 grade horizon karst caves and 3 grade terraces; 2) there are obvious different karst feature among different period of planation surfaces, such as the surface is integrated with lower peak cluster and karst basin and depression on the Exi Surface, but the karst feature changes in different areas on the Shanyuan Surface, which is dominated by peak cluster and gorge above the knick point and cone karst peak cluster and deep depression landscape with relatively integrated surface below the knick point; yet on the Pendi Surface, the morphology is dominated by peak cluster and uvala as well as valley; 3) the karst morphology once experienced 3 period s of evolution as the Exi period, Shanyuan period and Pendi period as well Xiagu period, which leading to the formation of the Exi and Shanyuan karst planation surfaces and the Pendi corrosion surface as well as the Xiagu gorge.
Progress of study on Mg/Ca and Sr/Ca ratios of speleothem in caves
ZHENG li-na, ZHOU Hou-yun, ZHU Zhao-yu
2010, 29(2): 201-218.
Abstract:
Trace elements in speleothem are important proxies of paleoclimate. In recent years, investigation on speleothem Mg/Ca and Sr/Ca ratios has got some important conclusions as follows: (1) Mg and Sr in speleothems derive mainly from overlying soil layer and wall rock. (2) Speleothem Mg/Ca and Sr/Ca ratios are able to indicate paleoclimate, but they should be explained in combination with other indices such as oxygen and carbon isotope ratios. (3) Speleothem Mg/Ca and Sr/Ca ratios are influenced by a variety of climatic and environmental parameters including the composition and features of overlying soil layer and wall rock, interaction between water and rock, advance carbonate deposit, distribution coefficients of Mg and Sr between solution and carbonate etc. Thus their interpretation is multiple depending on the dominant factor. (4) Mineral and crystallization also have certain influences on speleothem Mg/Ca and Sr/Ca ratios. Especially, it is easy to lost Mg and Sr during the transformation from aragonite to calcite,and lead to lower Mg/Ca and Sr/Ca ratios; incorporation of impurity would enhance inhibition of Mg and Sr into calcite lattice. In the future, more efforts should be paid in the mechanisms controlling migration of trace elements in speleothems, particularly in quantifying the connections between speleothem trace elements and forcing factors.
Study on detecting deep karst developing features by chemical tracing
HU Wei-yue, ZHENG Gang, YAN Lan-ying
2010, 29(2): 205-211. doi: 10.3969/j.issn.1001-4810.2010.02.016
Abstract:
Common received tracer concentration curve types are put forth and the corresponding relation between the received tracer distributing form and the karst features is studied in the paper according to karst developing features and the chemical tracer removing and diffusing regulation in karst aquifer. On this basis, in order to test the validity and practicability of chemical tracing in detecting karst developing features, the developing and the distributing features of the hidden katst in Ordovician limestone aquifer under the coal seam of Qiuji Mine, Shandong are analyzed, by putting the chemical tracer in surface drilling and receiving them from dewatering orifice under the mine. The results show, the strong developed Ordovician deep karst which spreads out along the direction of east and southeast from the northwest Qiuji Mine shows herringbone distribution patterns. The week developed and evenly distributed fissure karst takes dominant place in other area of the Qiuji Mine. It is found that karst developing distribution in the mine is conform to the water inrush from drilling hole in Ordovician limestone by compare hydrological data already made, which test the applicability and effectiveness of this technology.