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2014 Vol. 33, No. 1

Display Method:
Karst topography and hydro-geochemical characteristics in western Thailand and their correlation to that in southwestern China
ZHANG Cheng, JIANG Zhong-cheng, Mahippong Worakul, PU Jun-bing, Lü Yong
2014, 33(1): 1-8. doi: 10.3969/j.issn.1001-4810.2014.01.001
Abstract:
Thailand is situated in the central Indo-China Peninsula. The karst of Thailand is in the same global karst environmental zone as southwest China. Karst study in Thailand is mainly focused on the southern Shan states plateau in the north and Phang Nga bay of Karbi Province in the south. Published work on karst in Thailand has mainly been descriptive in nature, addressing topics such as the relationship between karst landscape development and regional geological structure in Mae Hong Song karst region, and the impact of climate, lithology and structure on coastline tower karst in southern Thailand. As yet, Earth System Science and Karst Dynamics have not been introduced into karst research in Thailand, thus research has not been carried out focusing on karst development mechanisms, influence factors. In this paper,the discussion of karst distribution and development,hydrogeological features of typical landscapes and their controlling factors in Thailand could help to promote study of correlations in karst geology between China and Indo-China Peninsula,providing fundamental support for the global karst carbon cycle monitoring network. Thailand has about 50,000 km2, of karst, i.e., one fourth of the Indo-China Peninsula. Typical karst landscapes are well developed, including plateau polje, peak cluster, peak valley and offshore peak forest. All those landscapes are important in the research field of global karst correlation. Since 2012, an international project in cooperation with the Department of Groundwater Resources of Thailand has been carried out by the Institute of Karst Geology. It is titled "Correlation study of karst geology between China and Indo-China Peninsula" and supported by China Geological Survey. Survey data indicates that karst in Thailand is mainly located in the west part in north-south direction, crossing 11 degrees (N19.3°to N8.5°) of latitude. Various karst landscapes with different hydro-geochemistry are found in the different latitude zone. At present, the first karst hydrogeological and carbon cycle monitoring station was established at Phu Toej spring, Kanchanaburi, Thailand, and high-resolution data was collected at 15-minute intervals for one year, including water temperature, pH, specific conductivity and dissolved oxygen. Compare to typical underground streams or springs in the karst of southwest China, Phu Toej spring has higher Ca2+(100-120 mg/L), HCO3- (8.6-9.3 mmol/L) and specific conductivity(700-777 μs/cm). This indicates that the intensity of karst processes in this catchment is much greater than that in the karst of southwest China, and there is potentially higher karst carbon sink intensity in such a tropical monsoon climate zone.
Evaluation of the potential groundwater resources in Tai’an urban-Jiuxian karst water system, Shandong Province
CHEN Wei-qing, WANG Yan-ling
2014, 33(1): 9-14. doi: 10.3969/j.issn.1001-4810.2014.01.002
Abstract:
Tai’an urban-Jiuxian karst water system is located at the foot of the southern Mount Tai in Shandong Province, it is a monoclinal structure water-bearing system with two water sources in urban and Jiuxian. It is higher in the north than in the south, covering an area of 112 square kilometers. The water-bearing stratum of the system are predominatly Quaternary, Cambrian and Ordovician, with a large area of Archaean igneous rocks of Taishan group in the south and the north. The tectonic unit is a part of Luxi anticline in the western Tailai fault subsidence basin. Faults include the NE-trending Taishan, Culaishan and Jiezhuang faults, and NW-trending Honggou, Panghe and Daidaoan faults. The water bearing formation includes a pore aquifer in uncosolidated Quaternary sediments and a karst bedrock fracture aquifer in the Cambrian- Ordovician carbonates. The groundwater is obviously affected by precipitation and artificial exploitation. By the end of 2012, the exploitation of groundwater was 52 thousand cubic meters per day, approaching the allowable with drawal limit of 57.9 thousand cubic meters, which is the equilibrium of exploitation and rechargement. Relying on the previous data, changes in the karst water recharge due to the barrage of Muwen River was studied. Results indicate that the system still has potential for exploitation due to recharge by surface water, and about 20 thousand cubic meters water per day are allowed to be exploited in the water-bearing system.
Study of the chemical features and geochemical susceptibility of the groundwater system in a typical karst trough valley
REN Kun, SHI Yang, LI Xiao-chun, LAN Jia-cheng, XU Shang-quan
2014, 33(1): 15-21. doi: 10.3969/j.issn.1001-4810.2014.01.003
Abstract:
The karst groundwater system is an important drinking water sources in karst regions. However, with urbanization development, groundwater in China has been widely polluted, especially karst groundwater in southwestern China. It is important to study the degree of response and mechanisms of groundwater features by external interference in order to guarantee drinking water safety. Using hydrochemical data for April 2012 to March 2013, the geochemical susceptibility of groundwater in Laolongdong subterranean river and Zhaojiayuanzi epi-karst spring in the river watershed of Nanshan, Chongqing was analyzed, and the principal cations were Ca2+ and Mg2+in the epi-karst spring, and Ca2+ and Na+ in the subterranean river. The principal anions were HCO3- and SO42- in both the subterranean river and the epi-karst spring. The values of Mg2+ / Ca2+and Na+ / Ca2+were greater in the dry season than in rainy season. The value of HCO3- / SO42- was 5.693-8.664 and 3.428-6.524 in dry season, 3.428-6.524 and 3.122-5.966 in rainy season. This indicates a high concentration of HCO3- and low concentration of SO42-. Owing to agricultural activities, the rank order of geochemical susceptivity for major elements in the epi-karst spring is HCO3-> SO42-> Ca2+> NO3- > Mg2+ > Na+ > K+ > Cl-. When agricultural activities, industrial activities as well as urban construction activities were all taken into account, the rank order of geochemical susceptivity for major elements in the subterranean river became HCO3- > Na+ > Ca2+ > K+ > Cl- > Mg2+ > NO3- > SO42-. With anthropic activities, each ion is becoming increasingly susceptive. Thus, more attention should be paid to karst groundwater pollution.
Comparison of comprehensive index method and fuzzy comprehensive method in the evaluation of groundwater quality: A case study in Zunyi City
LI Lu-juan, ZOU Sheng-zhang
2014, 33(1): 22-30. doi: 10.3969/j.issn.1001-4810.2014.01.004
Abstract:
The comprehensive index method and the fuzzy comprehensive method are widely used in groundwater quality evaluation. The groundwater environment in karst area is vulnerable and the potential pollution sources are complex. In order to better understand the effect of comprehensive index method and fuzzy comprehensive method in assessment of karst groundwater in Zunyi City, Guizhou Province, a typical karst area was selected for study. Applying comprehensive index method and fuzzy comprehensive method to evaluate and contrast analysis groundwater quality of nine representative water points in Zunyi, the results showed: The shallow groundwater quality in Zunyi is generally good, 33 % of the water was grade III or higher; but the individual regional groundwater quality is poor, mainly the NO2-, NH4+, Mn, Na+, Cl-, SO42-, total dissolved solids, total hardness (CaCO3) and Se exceeded the standard. There were six water points whose evaluation results were the same and all were grade II. The remaining three water points were different; in the comprehensive index method all were grade IV, while in the fuzzy comprehensive 2 water points were grade V and one water point was grade III. The main reasons for these differences are the maximum value of the single index are emphasized when calculate the comprehensive value F and the weight of evaluation indexes are not taken into account in the comprehensive index method; however, these disadvantages of the comprehensive index method are resolved in the fuzzy comprehensive method, the proximity of indexes to water quality classification limitation is carefully depicted, and the impact weight of all indexes to groundwater quality are quantified visible, so in the groundwater quality evaluation, the fuzzy comprehensive method is superior to the comprehensive index method.
Study of karst groundwater flow characteristics of a mine in Pingnan county, Guangxi through connection test
YU Le, WANG Li-heng, WANG Ju-ping
2014, 33(1): 31-36. doi: 10.3969/j.issn.1001-4810.2014.01.005
Abstract:
The mine in Pingnan county, Guangxi is located in a closed hydrogeological basin which borders the Qinchuan River in the east, the Xunjiang River in the south, the Wujiang River in the west and the watershed of groundwater in the north. The strata exposed in the mine area are mainly Devonian limestone and calcite dolomite, and Quaternary Holocene loose deposits. Declining groundwater levels due to artificial drainage lead to a redistribution of the groundwater flow field and the mining area became a cone of depression in the aquifer. The Qinchuan River is a potential risk to mining safety. In order to understand the flow path and percolation velocity of groundwater, and recharge sources of drainage water in the mine area, a connection test was conducted. The results of the connection test indicated that the medium of aquifer was highly heterogeneous and anisotropic because there was a huge difference in permeability between test sections. Moreover, the northern and eastern connectivity was better than that of the southern one. Groundwater velocity ranged from 0.3 to 20 m/h in the north and ranged from 3.72 to 98 m/h in the east. There is a groundwater watershed between the mine area and Xunjiang River, so the hydraulic connection of mine in the south and the periphery was weak. Therefore, the lateral runoff in the north and the leakage from the Qinchuan River were mainly recharge sources of groundwater in the first mining area based on the connection test results. In addition, except the lateral runoff in the north, local precipitation was the main recharge source for groundwater in the second mining area. Finally, in order to choose an appropriate time to drain groundwater, fluctuations in the level of Qinchuan River should be recorded and analyzed from a security perspective. On the other hand, some engineering measures should be considered to block groundwater flow, such as curtain grouting anti-seepage.
Experimental study of compressibility of red clay affected by acid-base and soluble salt solutions
GU Zhan-fei, LIU Qi, LU Yao-ru, LIU Zhi-kui
2014, 33(1): 37-43. doi: 10.3969/j.issn.1001-4810.2014.01.006
Abstract:
Guilin is located in the southwest of NE-SW trend Xiang-Gui lowland corridor with coordinates of longitude 110°17′and latitude 25°14′. It has a subtropical monsoon climate with abundant annual rainfall, and is hot, humid and rainy. Guilin is in the Lijiang River valley plain, which has well-developed karst and large areas of red clay. The engineering properties of red clay in Guilin are very complex, making the water stability poor. The chemical activity is closely related with the chemical composition of groundwater. To study the effects of the water environment on engineering geological properties, the red clay was taken from a typical karst area in Guilin. The samples were soaked in different concentration solutions of HCl, NaOH, Fe(NO3)3 and Al(NO3)3. Experimental results showed that:(1) The compression modulus of the red clay decreased and the compression coefficient increased when it was soaked in different concentration of HCl and NaOH solution, and that the greater the solution concentration was, the larger the decrease in range would be; (2) The compression modulus of the red clay was greater when the red clay was soaked in a solution of NaOH than that soaked in a solution of HCl, and the compression modulus value decreased with the increase of solution concentration, the opposite of the compression coefficient; (3) The compression modulus of the red clay increased and the compression coefficient decreased with the increase of solution concentration when the red clay was soaked in solutions of Fe(NO3)3 and Al(NO3)3,and the effect of the Fe(NO3)3 solution was greater than that of the Al(NO3)3 solution.
Numerical simulation research on the stability of transmission tower pile foundations in a karst area of Guangdong Province
HUA Shuai
2014, 33(1): 44-50. doi: 10.3969/j.issn.1001-4810.2014.01.007
Abstract:
The research on collaborative deformation of buried caves between transmission tower pile foundation in karst area occurred in Ruyuan county, Guangdong Province, China. The geological survey and drilling indicated that soils near the transmission tower are mainly alluvial silty clay, alluvial gravel, and residual silty clay. The bedrocks is predominately strongly weathered sandstone, moderately weathered quartz sandstone, limestone and carbonaceous limestone, which are generally greater than 30m in total thickness. Through drilling, nearly 10 different sizes of caves have been discovered in proximity to the tower. They are beaded or multi-layered in formation, and most are unfilled or half filled, where the overburden is normally 10-30 m, and a minimum of 1-4 m thick. The underlying caves have a large impact on the design, construction and operation of the transmission tower foundation. In order to study the stability and deformation of transmission tower foundations in this area, FLAC3D software was used for modele and calculations. By monitoring the stress, displacement and changes in the plastic zone at different positions, it showed that the stress distribution of the overlay is uniform and is minimally impacted by caves. However, the cave rock stress changes greatly. There is large bending down deformation in the roof of caves. Additionally, the bottom of the tower foundation moves down significantly, especially when a large stress loads are applied to the foundation and the cave roof, the cave roof would be unstable, leading to structural destruction of the pile foundation. The deformation characteristics of pile foundations with different rock-socketed depth indicate a positive correlation between rock-socketed depth and cave deformation.
Carbon sink effect of simulated acid rain in lime soil and carbonate rock system
LI Chun-long, ZHAO Jia-mei, LONG Si, CHEN Zhong-ji, ZHOU Yun-chao, ZHANG Chun-lai
2014, 33(1): 51-56. doi: 10.3969/j.issn.1001-4810.2014.01.008
Abstract:
In order to investigate the influence of rainfall acidity on the carbon sink in a lime soil and carbonate rock system, a leaching test was conducted using lime soil sample developed in pure limestone in Qingyan town and a pure limestone sample of Triassic Daye formation from Huaxi reservoir, Guiyang, comparing to the historical precipitation in Huaxi district, Guiyang. The influence of simulated acid rain on lime soil and the limestone system carbon sink was studied by measuring the HCO3- content, DOC in the leachates and the soil respiration rate in the lime soil and carbonate rocks system leached over six-months using a range of precipitation acidities and at various depths in the soil. The results showed that,(1) in the homogeneous sample in the soil of 10-50 cm deep , the content of HCO3- increased with increased thickness of soil, however the DOC content decreased and the rate of soil respiration increased, indicating that soil thickness significantly affected the carbon sink in the lime soil and carbonate rock system; (2) for pH values ranging 3.5-6.8, the samples had significant differences in carbon emissions increasing precipitation acidity inhibited karstification and organic carbon dissolution, and the karst carbon sink effect decreased;(3) for a daily precipitation range of 90-230 mm, the carbon sink was enhanced with the increased precipitation.
The records and implications of Mg, Sr and Ba in cave water and active speleothems in Jiguan Cave, western Henan Province
REN Xiao-feng, YANG Yan, PENG Tao, ZHAO Jing-yao, ZHANG Yin-huan, NIE Xu-dong, LIU Xiao, LI Jian-cang, LING Xin-you, ZHANG Zhi-qin
2014, 33(1): 57-63. doi: 10.3969/j.issn.1001-4810.2014.01.010
Abstract:
Speleothems contain a number of suitable proxies reconstructing climate environmental changes, which is a top topic in current research. Due to the variety of sources and complex factors, trace elements are less frequently used than the oxygen isotopes in climate studies. However, they are used to reveal the groundwater runoff in the epikarst overlying the cave with the process and the surface environment. Inductively coupled plasma mass spectrometry(ICP-MS) and inductively coupled plasma optical emission spectrometry(ICP-OES) have been used to analyse the trace elements of Ca、Mg、Sr and Ba in cave water and active formations in Jiguan Cave during December, 2009 and August, 2013. Jiguan Cave (33°46′ N,111°34′E) is located in Luanchuan county, western Henan Province, which is north of the Qinling ranges-Huaihe River and southeast of Loess Plateau, while at the foot of the northern watershed of the Yangtze River and the Yellow River. It main exposed rocks are Sinian chlorite marbles. Located in the typical east Asian monsoonal zone, the Jiguan Cave area is typically has cold/dry winters and warm/wet summers. More than 50 % of the total annual precipitation occurs in summer. The mean annual temperature and precipitation recorded at a nearby meteorological station are 12.1±0.9 ℃ and 846±181 mm (1957-2009) respectively. In the paper, trace elements such as Ca, Mg, Sr and Ba in cave water and active formations collected in Jiguan Cave were analyzed with ICP-MS and ICP-OES. The Mg/Ca, Sr/Ca and Ba/Ca of cave water varied between 0.2-0.8, (1.2-6.0)×10-3 and (0.3-2.0)×10-3 respectively. Mg/Ca can respond to the environment outside the cave faithfully. The wet-dry condition of the karst system is suggested as the dominant controller of Mg/Ca ratios in cave pool water and underground rivers, whereas the Sr/Ca and Ba/Ca may have nothing to do with precipitation and temperature. The Mg/Ca, Sr/Ca and Ba/Ca ratios in active speleothems varied between (9-50)×1010-3, (0.1-1.2)×10-3 and (0.8-3.2)×10-3 respectively. Corresponding to that of the water, the opposite trend was observed in Sr/Ca, Ba/Ca and Mg/Ca ratios. This opposite trend may have been influenced by atmospheric dust and surface soil, but there are still unexplained phenomenons worth further research. The co-precipitation coefficient constants for Mg/Ca and Sr/Ca between modern carbonate and water were calculated, giving a KSr value of 0.02-0.18 and KMg value of 0.01-0.03. Positive correlation between KMg and cave temperature is faint.
Geomorphologic value and contributions of the Huanjiang Karst Extension to South China Karst World Heritage
LIU Zi-qi, XIONG Kang-ning, LI Gao-cong, XIAO Shi-zhen, WANG Ling-yu, WANG Heng-song, LUO Ding
2014, 33(1): 64-76. doi: 10.3969/j.issn.1001-4810.2014.01.011
Abstract:
“South China Karst” is a serial World Natural Heritage site, nominated in phases by the government of China to the UNESCO World Heritage Committee. In this paper, based on the geomorphologic characteristic research of Huanjiang Karst, is compared with Libo Karst and other sites of “South China Karst”. It is concluded that: (1) Huanjiang Karst and Libo Karst have the same geomorphic landscape type-cone karst. (2) The extension adds the geomorphologic rejuvenation value to Libo Karst. (3) Huanjiang Karst in the nomination will make an important addition to the integrity problem about the boundary of the southern buffer zone of Libo Karst World Heritage Site, resulting from the administrative boundary between Guizhou and Guangxi Provinces, including geology and geomorphology, biology and ecology, natural landscape, etc., further more meeting the integrity requirements of world heritage; (4) In the history of South China karst, Libo-Huanjiang Karst recorded the sedimentary history of the second cycle of carbonate rocks. After experiencing the transformation processes of karst landforms from Dongwu, Indosinian and Neotectonic movements, they represent the cone karst landform in the transition zone from the Yunnan-Guizhou Plateau to the Guilin Basin in southern China and the ongoing evolution process of cone karst geomorphology. It is the model site for tropical-subtropical cone karst in the world.
The drought stress and rehydration influence on chlorophyll fluorescence characteristics of Barbula fallax Hedw. in areas of karst rocky desertification: Case study near Huaxi district, Guiyang City
ZHANG Xian-qiang, WANG Shi-jie, SUN Min
2014, 33(1): 77-81. doi: 10.3969/j.issn.1001-4810.2014.01.012
Abstract:
Guiyang city is located in the central Guizhou Province, at an average elevation of 1 100 m, annual average temperature 15.2 ℃ and annual average rainfall of 1 178 mm. The soil in Guiyang is predominately calcareous (accounting for 85 %), whose parent rocks are mainly dolomitic limestone and calcium dolomite. Its forest coverage is 5 %-15 %, the vegetation coverage is 10 %-90 %, the bare rock is 30 %-90 %, the land reclamation is 10 %-70 %, and the average rocky desertification is 36.79 %. Huaxi district in Guiyang is taken as an example for ecological restoration and treatment research, which provides the basis for scientific selection of drought-resistant plants for cultivation in karst rocky desertificationareas. Chlorophyll-fluorescence was measured by a handy PAM-2100 fluorometer in moss Barbula fallax Hedw. when drought and rehydration affected chlorophyll content and fluorescence under increased drought stress, the total chlorophyll content first dropped , and then increased gradually. F0 and qN of three kinds of mosses increased while the Fm , Fv/Fm, Yield, ETR and qP decreased with drought stress. Fluorescence parameters after rehydration were restored to normal levels by mild to moderate stress, and severe stress is more difficult to return to the control level. 
Ecosystem constitute pattern and change evaluation to karst mountain base on RS and GIS: A case study in Bijie, Guizhou Province
LI Xue-dong, YANG Guang-bin, ZHANG Xu-ya, LI Bing, WANG Mao-yang
2014, 33(1): 82-90. doi: 10.3969/j.issn.1001-4810.2014.01.013
Abstract:
Bijie City, Guizhou Province is located in slope zone between the eastern Yunnan plateau and Qianzhong tableland and hills, which is a typical karst area. Bijie region consists of Dafang, Qianxi, Jinsha, Zhijin, Nayong, Hezhang and Weining counties and Bijie City. It has a fragile ecological environment. In order to better understand Bijie ecosystem composition, structure and change characteristics, in this paper, based on object-oriented classification and spatial statistics and analysis technology, the ecological system of Bijie prefecture in 2000 and 2010 was extracted from Landsat TM image, and the ecosystem composition, structure and characteristics were analyzed quantitatively. The results showed that: from the view of the ecosystem composition and structure, the study area in 2010 was mainly composed of forest land and farmland ecosystem types, accounting for 42.65 % and 42.65 % respectively; in 2000 and 2010, the region had a higher number of patches and the smaller average patches area, indicating a higher degree of landscape fragmentation in the region. Number of patches in 2010 was less than that in 2000, indicating that the study area landscape connectivity was improved totally, the whole landscape tended to be neat. The dry land patches and the average plaque area decreased in 2010, while the coniferous forest and grassland increased, showing that the Grain for Green project worked; The dry land and coniferous forest concentration increased, which indicated that connectivity was enhanced and the landscape became more concentrated. Depending on the statistics of conversion area of ecosystem during 2000 and 2010, the total conversion area of all ecosystem types in the study area was 1 298.25 km2, the upland and paddy field area decreased significantly, the woodland and grassland increased obviously, the land transfer matrix displayed that dryland mainly became forestland or grassland. Due to larger drought area, the area in Bijie, Qianxi, Dafang changed greatly and the ecological transformation intensiy are high, the ecological system type transformation intensity values of eight administrative area were positive, showing that the ecosystem cover types tended to be improving.
Species diversity of rare and endangered species and endemic species and conservation of Guilin Karst World Heritage Nominated Property
SHEN Li-na, HOU Man-fu, ZHANG Yuan-hai, CHEN Wei-hai, XIANG Chui-sheng, LI Xiao-na
2014, 33(1): 91-98. doi: 10.3969/j.issn.1001-4810.2014.01.014
Abstract:
Rare and endangered species, and endemic species are important to regional biological species composition. Rare and endangered species, and endemic species biodiversity research is very significant for biological conservation and maintaining the ecological environment. The rare and endangered species, and endemic species of Guilin Karst World Natural Heritage nominated area are statistical analysis based on species investigation. Conservation suggestions of rare and endangered species, endemic species are proposed in 3 levels: population, community and habitat. The results of species diversity investigation suggest that: 754 species of high plants and 525 species of vertebrate animals have been found in 16,750 ha area. Including 443 species in IUCN Species Red List, 67 species in the Conventional International Trade in Endangered Species of Wild Fauna and Flora (CITES), and 145 species in China Species Red List,and 55 species listed as China national key protected wild plants and animals. There are some relic plants, rare and endangered species with high diversity. There are 87 endemic species, which are important endemic species source. For biodiversity conservation of rare and endangered species and endemic species, population investigation and habitat analysis should be done based on level of threat of rare and endangered species. The minimum viable population and minimum dynamic area of rare and endangered species should be determined. In situ conservation or ex situ conservation is used for developing minimum viable population. Climax community conservation and monitoring research are enhanced as well as close hillsides to facilitate afforestation and community restoration project are carried on. Nature protection area is established for maintaining species survival and multiply essential habitat. Furthermore, wild orchid research and living space conservation should be enhanced as well as unique habitat conservation for cave, peak forest, cliff.
Analysis on the structure features and types of the rural settlement in karst mountain:A case in Wushan county,Chongqing
MIN Jie, YANG Qing-yuan
2014, 33(1): 99-109. doi: 10.3969/j.issn.1001-4810.2014.01.015
Abstract:
China has entered a new period of building well-off society in an all-around way, which includes karst mountain where is sparing no effort in developing the rural construction level. It is of very important significance to analyze the special spatial distribution characteristics of the rural settlement in karst mountain for optimizing the rural settlement spatial layout and promoting the construction of a new socialist countryside and the integration of urban and rural development. In order to explore the spatial characteristics of the rural settlements in karst mountain, in light of special metrics modles of distribution, dimension and shape,the paper conducts a quantitative analysis on the space differentiation of rural settlements in Wushan county, and further identifies the regional types. The results are as follows. As a whole, in spatial distribution the rural settlements in Wushan are of certain concentrating features but exist obvious regional difference. The rural settlements are of low value congregation features and are small in scale generally. In spatial form, the rural settlements in the west Wushan are characterized by good connectivity and high complex but irregular in shape; those in the east Wushan are characterized by poor connectivity and low complex. Overall, the rural settlements are characterized by low irregular shape in need of planning and adapting. By means of constructing space measurement index system of the rural settlements with the hierarchical cluster method, six types of rural settlement in Wushan are divided as follows: low-density point-scattered type, low-density small-mass type, medium-density stripe type, low-density irregular-mass type and high-density wide band type as well as high-density point-scattered type. Rural settlement reconstruction works in the future should be guided by the characteristics of different types.
Features and exploitation of karst cave tourism resources in Jiangxi Province
HE Xiao-qian
2014, 33(1): 111-117. doi: 10.3969/j.issn.1001-4810.2014.01.017
Abstract:
Exploitation and utilization of karst caves is the focus of show caves, and the rational use of karst caves plays an important role in promoting the development of regional tourism industry. Jiangxi Province lies on the southern bank of the middle reaches of the Yangtze River. It has a total area of 166,900 square kilometers and contains rich ecotourism resources, with a coverage rate of up to 90 %. The landforms in Jiangxia relatively complete, located in an irregular ring structure, and are mainly comprised of mountains and hills. The epi-karst are mainly characterized by karst hills, residual hills, isolated hills, stone teeth, karren, karst doline and karst depression without peculiar formations. However, the endo-karst have a wonderful array of shapes and formations, which is one of the dominant tourism resources in Jiangxi. Relying on the collected data and some fieldwork, karst cave distribution and features were analyzed and the tourism development model and countermeasures were discussed. Thirty-one show caves are located throughout 28 counties of 9 cities, and concentrated in the northeast and the west of the province. The cave landscapes are peculiar and some have a long history of development with high scientific and cultural value. According to a comprehensive analysis of the main tourism factors such as show caves’ features, locations, regional economic development, the development pattern of show caves in Jiangxi may be classified into three types: independent, combined and supporting. The developed countermeasures are correspondingly themed development, reasonable travel planning, combining karst cave tourism and exploration and tourism promotion.
Application analysis of combining high density resistivity and microtremor survey methods in areas of karst collapse:A case study of the collapse in Jili village, Laibin, Guangxi
LIU Wei, GAN Fu-ping, ZHAO Wei, CHEN Yu-ling
2014, 33(1): 118-122. doi: 10.3969/j.issn.1001-4810.2014.01.018
Abstract:
In order to verify the applicability of geophysical prospecting technology to the investigation of karst collapse, the field research was carried out employing high density resistivity and micro technology methods in Jili village, Laibin City, Guangxi. It showed that the high density symmetric quadrupole sounding method intuitively reflected the thickness of the Quaternary overburden layer and the depth of the low resistivity section underground, while micro technology qualitatively analyzed the surface projection of the underground river and karst fracture zone. This would be more accurate in the case of circling collapse and unfavorable geologic bodies which caused collapse, such as caves, underground rivers, fault fracture zones and soft soil by combing two methods. It also showed that a low resistivity orthogonal point appeared in the high density profiling curve and its value was about 250 Ω?m when the polar distance was 45 m while a great value anomaly appeared on the H/V spectrum and the maximum characteristic frequency was in the range of 2-6 Hz above the underground river or karst fracture zone. On the basis of anomalies in the high density resistivity method and micro method of the line 2, the two sections circled were easy to collapse and one selected to be verified by drilling. Drilling revealed eight caves in limestone covered by a 42 m thick Quaternary overburden, of which the largest cave was up to 5.7 m in height.