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2010 Vol. 29, No. 4

Display Method:
Progresses and important activities of karst research during the 11th Five-Year Plan in China
JIANG Zhong-cheng, PEI Jian-guo, XIA Ri-yuan, ZHANG Mei-liang, LEI Ming-tang
2010, 29(4): 349-354. doi: 10.3969/j.issn.1001-4810.2010.04.001
Abstract:
International karst research center is founded in Guilin and fruitful progresses both in theory and practice research have been got during the 11th Five-Year Plan. Theoretically, the karst dynamics is developed in light of the earth system science views and modern automatic testing measures. And the new growing point, karst ecology not only has brought to light the fragility of the karst eco-system and the changes in soil quality as well as the speciation law of some soil nutrient elements in southwest China, but also selected a lot of special species that suit the karst environments. In the field of global change researches, the dissolved in organic carbon of the karst hydro-cycle has been found as an important part in global carbon cycle and many climatic supersede indicators has been used to deepen the study on palaeo-environmental records of the cave stalagmites. Furthermore, new technology and soft ware is used to study the available evaluation methods in the water quality and quantity evaluation of karst underground water. Practically, the geological survey data, including the karst water resources in southwest China and the karst rocky desertification environments as well as the soil erosion datum, has played important role in the national goal and significant society demands on one hand. And on the other hand, typical geo-model is formed in the gas and oil exploration in karst areas, the South China Karst is reported and listed successfully as the world natural heritage and the new monitor and early warning techniques of karst collapse are successfully used to prevent and cure karst collapse in the practical engineering.
Progress of research on rocky desertification in South China Karst Mountain
XIONG Ping-sheng, YUAN Dao-xian, XIE Shi-you
2010, 29(4): 355-362. doi: 10.3969/j.issn.1001-4810.2010.04.002
Abstract:
Based on the research on rocky desertification of the previous scholars, the actual state of research on rock desertification in South China Karst Mountain is reviewed in this paper from the concept connotation of rocky desertification, distribution pattern and quality grading, cause analysis and forming process, integrated control and effectiveness evaluation and so on. Consensus for the concept and formation cause of rocky desertification have already been reached, but the classification evaluation grade index of rocky desertification are different with each other, so general investigation method, unite classification index and appraise index system should be build. Although a few fairly good comprehensive models and methods have already been proposed, there is still no mature methods and effects evaluation system for desertification controlling, which affects the revision and improvement for governing measures of rocky desertification seriously. So, it is proposed that the researching works should be enhanced in the following respects: innovating the research methods, keeping the interaction of rocky desertification and human impacts in hand, enhancing the study on the process simulation and control measures of karst rocky desertification, popularizing and improving comprehensive treatment technique of karst rocky desertification, and paying special attention to use the geosystem science in karst rocky desertification. Furthermore, in the field of the interaction between rocky desertification and human impacts, it is particularly necessary to stress the quantify research for land productivity and bearing capability, to forecast the effects of human economic activity and economy society consequence to establish ecological security monitor and pre-warning information system in karst mountain, to enhance the study on artificial drive mechanism of differential space-time dimension in the future, to distinguish the effects and contribution rates to rock desertification process between natural and human factors respectively, and to build corresponding concept model and mathematic model.
Distribution of organichlorine pesticide in the water and sediment of the Bailang Subterranean Stream in Guangxi
KONG Xiang-sheng, QI Shi-hua, Oramah I T, ZHANG Yuan, HUANG Bao-jian
2010, 29(4): 363-371. doi: 10.3969/j.issn.1001-4810.2010.04.003
Abstract:
In order to understand distribution of organochlorine pesticide in the water and sediments of the Bailang Subterranean Stream in typical karst area in Leye, Guangxi, the water and sediment samples on different sections are collected and 19 kinds of OCPs are detected with GC-ECD. The results show that,(1)The total organochlorine pesticides concentration(∑OCPs) in the surface water of the Bailang subterranean stream ranges from 1.95 to 71.45ng/L, the concentration of HCHs ranges from undetectable to 58.40ng/L, and DDTs undetectable to 0.44ng/L respectively. (2)The concentration of∑OCPs in the sediment ranges from 0.75 to 14.85ng/L, HCHs from 0.11 to 3.52ng/L, and DDTs from 0.03 to 2.90ng/L. (3)Distributions of OCPs in water and sediment from the Bailang Subterranean Stream are related with adsorption, temperature and the soil erosion at the bottom of Tiankeng where connected with subterranean stream. Namely, OCPs of atmospheric sedimentation is easily gathered in soil at the bottom of Tiankeng for temperature difference effect (this is “cool trap effect”), and then, OCPs moves toward the water body so that concentration of ∑OCPs in sediment of the subterranean stream increases. (4)It is inferred that the OCPs in the sediment of the subterranean stream could be released to cause secondary pollution for the value of the sediment adsorption coefficient being lowest at the exit of the stream, but higher in concentration and kinds of OCPs in the stream water. (5)The ecological risk is at the low risk due to concentrations of the endrin on most sections and both DDTs and DDD on the section of the Leye County surrounding areas range between effects range to low(ERL) and effects range to median(ERM). (6)There are both newly HCHs and DDTs inputs recently on some sections. Organochlorine pesticide has accumulated for along time, which may be cause harm to the underground river ecosystem. Therefore, local government should take preventive measure.
Assessment on the antifouling property of karst ground water in Huaibei City
ZHANG Xin, HE Jiang-tao, WANG Jun-jie, Li Peng
2010, 29(4): 372-377. doi: 10.3969/j.issn.1001-4810.2010.04.004
Abstract:
The antifouling property of karst ground water in Huaibei City is assessed by means of PI (protective layer and infiltration condition) method on the basis of deep study to regional hydrogeologic conditions, in order to protect and rationally exploit the karst ground water resources. The results show that the region with antifouling property value π that less than 2 locates in low mountains and hills, where is rock outcrop area with the bedrock buried within 50m in depth; that the value π between 2 to 3 mainly distributes in hills, residual hills and piedmonts, where are rock covered area with the bedrock buried in 50~200m; the value π that more than 4 locates in the plains is buried area with the bedrock buried deeper than 200m under the ground. Either the PI evaluation results or the geologic conditions of assessment object show that the antifouling property of the karst ground water in mountains and hills is week or relatively week and gets stronger with the distance away from the mountain, and the antifouling property is best in plain.
Numerical simulation for the evolution of the overflow spring in fracture-karst aquifer system
WANG Yun, YU Qing-chun, MA Hao
2010, 29(4): 378-384. doi: 10.3969/j.issn.1001-4810.2010.04.005
Abstract:
Based on discontinuous fracture network medium model, coupled hydrodynamic conditions and the dynamic conditions of carbonate dissolution, this paper established a mathematical model and take numerical method to simulate and analyze the evolution of fracture-karst aquifer system. On the basis of established numerical model, two sets of instance model are constructed(one fracture-karst aquifer system recharged by precipitation and the other one recharged by river) to study the early evolution of overflow spring in the fracture-karst system. It is found that with the evolution of fracture-karst aquifer system, the fractures are constantly corroded and widened, which lead to water table declines and many springs being drained out. Moreover, since the variance dissolution, corrosions are quicker at the water table and in the vicinity of the dominant fracture, while the other location is relatively slow, and a karst dominant tube is gradually formed which captures most of the water in the system and develops large spring. Comparing the two instance models, it is also found that in rainfall infiltration recharged system, the springs develop from the sink to the source; while in river infiltration recharged system, the springs develop from the source to the sink.
2010, 29(4): 384-384.
Abstract:
Analysis on the development characteristic of the Luoma Cave Underground River and the origin of the flood
HUANG Kun, WU Ya-zun, WAN Jun-wei, XIAO Pan
2010, 29(4): 385-388. doi: 10.3969/j.issn.1001-4810.2010.04.006
Abstract:
According to the karst development history in the region, the formation and development of the Luoma Cave Subterranean River can be divided into two stages. The first stage occurred from the end of the Cretaceous Period to the late Tertiary Period. In this phase, precipitation was caught into the karst under-ground pipeline through the small karst depression and sinkholes located by the sides of the Woxiping polje, then drained into Woxiping polje and formed a small karst lake, and 3 east-westwards underground rivers formed at the same time. The second phase occurred from the end of the Tertiary Period until now. During this stage, with the uplift of the regional oscillated structure motion, the erosion base level declined continually. The Xiaheicao, Tongluoping and Woxiping sinkholes formed, and the east-west wards pipelines that formed in the early phase were transfixed and then the new pipeline captured the water from the karst lake, which made the dispersive karst water system discharged focused through the south-north wards pipeline and formed multi-entrance dendritic underground river system. The scale of the Luoma Underground River which formed in the later periodis too small and highly filled up that led to the discharging capacity get diminished, which is the main causation of the flood disaster in the polje. Based on this analysis, the governing way of the flood disaster in the drainage basin should include enhancing management of soil erosion, dredge river way and build new drainage tunnel.
Grey system analysis software development for karst ground water modeling
WANG Ya-jie, HAO Yong-hong, WANG Xue-meng, LI Hua-min, ZHAO Jiao-juan
2010, 29(4): 389-395. doi: 10.3969/j.issn.1001-4810.2010.04.007
Abstract:
After analyzed recent application of grey system theory in karst hydrology, a grey system modeling software is developed by means of step wise refinement method and VisualC++ 6.0 with the thoughts of software engineering. There are six modules in the software including grey relational analysis, data pretreatment, grey relational analysis, GM(1,1) model, dimension-fixed and recursion-compensated prediction model, GM(1,1) decomposition model, and GM(1,N) model as well. It is object-oriented and easy to operate, and able to meet the needs of hydrologists for groundwater simulation. This paper describes the software's design process, analyzes the functions and implementation of each module, presents the software examination process, and states the software's benefits on the basis of a case study in Liulin Springs, Shanxi, China. AGM(1,1) model is set up for Liulin Springs in light of the spring discharge data from 1971 to 2007, and the model is verified by spring discharge data in 2008 and 2009. The results show that the residuals errors decrease from 0.32 m3/s to 0.17m3/s in 2008 and from 0.29m3/s to 0.19m3/s in 2009 by periodic correction to the residuals.
Preliminary research on climate evolution and driving mechanism during the Middle Holocene in Xundian, Yunnan
ZHANG hui-ling, QIN Jia-ming, PU Xiao-qiang
2010, 29(4): 396-401. doi: 10.3969/j.issn.1001-4810.2010.04.008
Abstract:
By dating ages of TIMS-U series and analyzing carbon and oxygen isotope and content of organic carbon in XR1 stalagmite from Xianren Cave in Xundian, Yunnan, the paper reconstructs monsoon climate change pattern during the middle Holocene in Xundian. It can be divided into three climate periods approximately: (1)8.0~6.0ka B.P. was warm and wet period; (2)6.0~5.1ka B.P. was climate change period. During the period, climate changed from wet and warm to cold and dry; (3)5.1~2.1ka B.P. was climate recovering period. In the period, the climate changed from cold and dry to the average climate level of the Middle Holocene. After contrasting organic carbon variation to δ18O record, it reveals that organic carbon in stalagmite can reflect climate change. But organic carbon variation lags to climate change. At last, on the basis of δ18O record and summer solar radiation at 33°N latitude, the driven factors of climate change in Xundian, Yunnan Province during the mid-Holocene is analyzed. The result show the climatic changing trend in Xundian, Yunnan Province was controlled by summer solar radiation at 33°N latitude and may affected by volcanic activity during the mid-Holocene.
Palaeo-karst development model of the Pre-Tertiary carbonate rock in Jizhong Depression
WU Kong-you, WANG Yu-jie, LI Zhu-qiang
2010, 29(4): 402-409. doi: 10.3969/j.issn.1001-4810.2010.04.009
Abstract:
The formation of the Pre-Tertiary carbonate rocks in Jizhong Depression has gone through multi-phase karstifications. In light of the formation time, cause, and the morph character of the palaeo-karst, 5 models of Palaeo-karstification are recognized as syngenetic karst formed in the interlayer during the formation of the rocks, supergene karst formed in weathered crust during denudation, fracture karst formed in fractures or joints during denudation period, phreatic karst formed under the released water and thermal fluid condision. The former three kinds of karst are superficial karst and controlled by geo-structures and sea level fluctuation, they are the basis for the development of the reservoir stratum. The latter two, belonging to buried karst that relating to acidic fluid and under ground thermal fluid, have remolded the erosion holes in the former weathered crust and formed the major and direct factors for the development of the reservoir stratum. The development and distribution of the karst fissure and cave system is controlled by the multi-phase karstification, so the paleo-karstifications are of important geologic significance for the formation of the reservoir stratum.
Study on response of carbonate rock dissolution rate to the season in Zhongliang Mountain, Chongqing
XIE Fang, FU Wa-li, WANG Xiao-yang, PU Peng, ZHANG Lei, TAN Bo, PENG Jing-tao, HEN Xiao-jun
2010, 29(4): 410-413. doi: 10.3969/j.issn.1001-4810.2010.04.010
Abstract:
Taking the karst area of Zhongliang Mountain as a case study, response relation of dolomitic limestone solution rate under different land using tapes to the season is analyzed through solution rate test on Jialingjiang dolomitic limestone piece of lower Triassic System in the field. In the test, four different types of land use, wood land, orchard land, farmland and vegetable field are chosen. The results indicate that the soil properties are highly different with the change of land use types, which affect the dissolution rate obviously. Both in summer and the whole year, dissolution rates under different land use tapes are (from high to low) wood land, vegetable land, farmland and orchard land. The dissolution amount in summer accounts for more than 50% of that in the whole year. And the dissolution rate in summer is higher than the average rate in whole year, except that in the 50cm deep in the wood land, vegetable field and orchard land. The reason is that the CO2 and moisture increase in summer because of the high temperature and more rainfall, which are in favor of solution.
Study on the regime of eco-efficiency in Guizhou Karst Area
YANG Ting-feng
2010, 29(4): 414-418. doi: 10.3969/j.issn.1001-4810.2010.04.011
Abstract:
To improve the eco-efficiency is an important point for the realization of regional sustainable development. In order to quantitatively understand the regime of the eco-efficiency in Guizhou karst area,the regime of the eco-efficiency is analyzed by the single ratio method based on eco-footprint model, and history data from 1978 to 2009 is used in the analysis. The results show that eco-efficiency increase in the research period from 288.249 yuan GDP/hm2 to 3 006.220 yuan GDP/hm2, and the average annual growth is 84.937 yuan GDP/hm2. But compared with the whole country, the eco-efficiency is always lower and the gap gets bigger and bigger, from 346.837 yuan GDP/hm2 in 1978 to 3242.609 yuan GD P/hm2 in 2009 and the average annual growth of the gap is 90.439 yuan GDP/hm2. On the above basis, some countermeasures to improve the eco-efficiency are put forward, fully exerting regional advantages; actively adjusting the energy structure; strengthening the recovery and comprehensive utilization of the “three wastes”; saving land and water resources; promoting industry ecologicalization and increasing economic benefit.
Research on control way for cultivated land in karst rocky desertification basin—A case in Shiqiao Basin, Bijie City and Mugong Basin, Guanling City in Guizhou Province
ZHOU We, XIONG Kang-ning, GAO Jian-fei
2010, 29(4): 419-424. doi: 10.3969/j.issn.1001-4810.2010.04.012
Abstract:
Shiqiao Basin in Bijie City and Mugong Basin in Guanling City in Guizhou Province are karst rocky mountain areas with strong rocky desertification, high density of population, and low and instable grain yield as well as low agricultural economic level. Through forecasting the increase trend of the population and using the human-land balance model, the necessary farmlands for these two basins have been counted as 281.91 hm2 and 228.68 hm2, However, the area of necessary farmland is larger than non-desertification farm-land, which leads to rocky desertification still appear in the farmland. If the grain for green project has been carried out in this place, it will not meet the need for food. Therefore, the measures as intercropping of trees and crops, crop-grass intercropping, reforming sloping fields to terraced fields have been carried out. As a result, rocky desertification has been controlled and soil erosion modulus of the two basins has decreased from 721.63t/(km2?a) and 42.42t/(km2?a) in 2007 to 472.78t/(km2?a) and 35.59t/(km2?a) in 2009, vegetation covered lands have increased by 11.3% and 6.4%, per capital income has increased by 300 Yuan and 231 Yuan. Rocky desertification has been controlled as well as peasants have got much more livelihood safety.
Regime of vegetation coverage in Lianjiang Watershed in North Guangdong Karst Mountain
WANG Xi-zhi, GAN Chun-ying, LIANG Zhao-xiong, GAO Quan-zhou
2010, 29(4): 425-433. doi: 10.3969/j.issn.1001-4810.2010.04.013
Abstract:
The spatial and temporal regimes of the vegetation cover from 2001 to 2010 in the Lianjiang Watershed are analyzed by means of the multi-temporal MODIS-NDVI and GIS and the dimidiate pixel model techniques in this paper. The results show that there is obvious otherness in vegetation covers between the Lianjiang watershed and its sub-streams and between karst and non-karst areas; and the vegetation coverage keeps decreasing in the recent 10 years with the high coverage and medium coverage areas undulating sharply, but the comparatively high or low coverage areas keeping stable. The karst area are mainly composed of high(53.84%), medium(25.59%) and comparatively high(18.54%) vegetation coverage, but comparatively high(48.12%), comparatively high(34.10%) and medium(15.05%) in no-karst area. The vegetation coverage has been clearly decreased in the recent 10 years as a whole and the vegetation coverage decreasing area is 20% more than the increasing area.
Preliminary study on spatial heterogeneity of soil mineral composition and organic carbon content at different micro-habitats that under different vegetation types in karst region
LIAO Hong-kai, LONG Jian, LI Juan, YANG Jiang-jiang, FENG Ye-qiang
2010, 29(4): 434-439. doi: 10.3969/j.issn.1001-4810.2010.04.014
Abstract:
The spatial heterogeneity of soil mineral composition and soil organic carbon (SOC) are determined through sampling at 7 kinds of micro-habitats, including soil surface, rocky surface, stone crevice, stone gully, stone cavern and stone groove as well as stone pit, under different vegetation cover, arbor and shrub and grass as well, in karst region. The results prove that, (1) The composition of soil mineral is diversity under different vegetation types. Quartz and kaolinite in the soil do not change under grass and shrub as well as arbor vegetation cover, dolomite in the soil in grass land disappears, and chlorite gradually appears in the shrub and arbor forest. (2) With the vegetation succession, the content of SOC significantly increases, and the content of micro-habitats SOC shows evident heterogeneity as follows: grassland > arbor forest > shrub land. Moreover, taking the content of SOC and the coefficient of variation at micro-habitats as evaluation factors, cluster analysis to the SOC under arbor forest and shrub as well as glass covers is done. The results show that the micro-topography is very important factor affecting the content of SOC and its spatial heterogeneity. To protect the SOC, the major work is improving vegetation covered ratio in grass and shrub vegetation cover areas, and keeping the good conditions of vegetation and decreasing human interference in the arbor vegetation cover areas.
The migration of elements among rock, soil and vegetation in karst area—A case in karst hilly area in Bama, Guangxi
MO Yuan-fu, XI Xiao-shuang, CHEN Zhong-jiang
2010, 29(4): 440-444. doi: 10.3969/j.issn.1001-4810.2010.04.015
Abstract:
Through the analysis on the elements relation ship and element removal between carbonate rocks and the soil, between carbonate rocks and vegetation (Alchornea trewioides and Callicarpa nudiflora Hook et Arn), and between soil and vegetation (Alchornea trewioides and Callicarpa nudiflora Hook et Arn). The study finds that, 1)there isa high correlativity between the rock and soil with the general removal sequenceas CaO>MgO>Na2O>P2O5>MnO>Pb>Zr>Fe2O3>TiO2>SiO2>Al2O3 from the rock to the soil; 2)there is also a high correlativity between the soil and the 2 species of tested plant, and the plants get similar element absorption coefficient from the soil, with the sequence of element absorption coefficient of the Alchornea trewioides being P>Ca>Fe>K>Na>Mn>Pb>Al>Mg>Zr>Ti>SiO2, and that of the Callicarpa nudiflora Hook et Arn being P>K>Fe>Na>Ca>Mn>Al>Pb>Mg>Zr>Ti>SiO2; Element migration follow certain rules. That is, rock elements are high correlated with soil elements. From rock to soil, the general element migration sequence is CaO>MgO>Na2O>P2O5>MnO>Pb>Zr>Fe2O3>TiO2>SiO2>Al2O3. 3)the macro-element implants are determined by the rock, so there is higher correlativity and consistency in the elemental composition of the plant growing under the same lithology.
The main eco-environmental problems and prevent measures within the watercourse-type fluctuation zone—A case in Chongqing reach of the Three Gorges Reservoir
SU Wei-ci, ZHANG Jun-yi
2010, 29(4): 445-450. doi: 10.3969/j.issn.1001-4810.2010.04.016
Abstract:
With the Three Gorges Reservoir being completed, a watercourse-type fluctuation zone with up to 30m high fall is going to appear, which will bring about a large periodic wet lands ecosystem. According to the water-store planning of the Three Gorges Reservoir and the particular characteristics of the fluctuation zone, important eco-environmental issues, such as eutrophication caused by land use, the near shore pollution in back water area, and the water pollution by ship's navigation, are discussed in the paper. Furthermore, in light of the reason and spatial-temporal distribution as well as development tendency of the above problems, it is proposed that the following prevention and control measures should be adopted, to evaluate the suitability of land use in the fluctuation zone, to reclaim the land step by step, to establish ecologic protective barrier, to carry out controlling engineer to domestic sewage and industrial pollution and domestic garbage, and to develop environmentally friendly recycling eco-agriculture, as well as to establish monitoring and warning system for the eco-environment in the fluctuation zone through the 3S technique.
Tourism environmental capacity of Wujiang Karst National Geopark in Sinan County, Guizhou Province — A case in stone forest scenic spot
ZHANG Hong-chao, ZENG Ke-feng, WAN Neng
2010, 29(4): 451-456. doi: 10.3969/j.issn.1001-4810.2010.04.017
Abstract:
Based on the summary of the research progress at home and abroad and in light of linear total amount model and planar total amount model, the environmental capacity of the stone forest in Sinan is comprehensively studied from 4 aspects, that is, space environment capacity, ecological environment capacity, economic capacity and psychological capacity. Finally, a reasonable environment capacity of the stone forest in Sinan is identified, that is the number of tourists should be7 298 in the boom season, 3 649 in the off season and the environmental capacity of the year be 1.824 5 million according to “Buckets effect”. On the above basis, it is proposed that 3 kinds of measures, traveling route, dining characteristics and management style, should be adopted to adjust the people and vehicle proportion, the timely traffic flow and the tourist automatic flow, which are the ways to realize the reasonable distribution of tourist and fully utilization of the infrastructure in the scenic spot.
Research on settlement culture type and the characteristics in Guizhou Karst Area
ZHAO Xing
2010, 29(4): 457-462. doi: 10.3969/j.issn.1001-4810.2010.04.018
Abstract:
This paper discusses composing factors and cultural layers of the settlement culture in Guizhou Karst Area in view of karst human-environment relationship. And then categorizes the settlement culture into 6 main types according to regional differentiation rules and combination of comprehensive analysis and leading factors. The major types involve valley settlements, hills ettlements, brook settlements, plain settlements and cave settlements as well as military outpost settlements. Special scattered pattern of the settlement is formed in karst valleys for the small space size and low environment capacity; influenced by the hill environment, typical hanging house or the Diaojiaolou is buil tc omplying with terrain in middle hill settlement, which forms the local architecture features; bead-string-shaped distribution along the river banks is formed in brook settlement for the higher environment capacity in the karst basin or valley; in plateau area, for the higher environment capacity and open space, multi national people live together and intensive village pattern settlement with frequently cultural exchanges is formed; because of the particularity of the cave environment, small settlement pattern is formed complying with the caves in cave settlement area; influenced by karst environment and human history, military outpost settlement culture mingled with the stone culture, Jiangnan culture and military cultural. This paper reveals the characteristics of different types of settlement, including settlement scale, settlement layout, settlement environment and building as well as life-style, in order to provide reference for exploiting Guizhou karst settlement culture rationally.