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2016 Vol. 35, No. 3

Display Method:
Tracer tests for pollutant sources of the Zengpiyan remainder cave in Guilin, China
ZENG Xin-ru, JIANG Guang-hui, GUO Fang, TANG Qing-jia, LIU Fan
2016, 35(3): 245-253. doi: 10.11932/karst20160301
Abstract:
The composition and source of groundwater pollutant are complex around Zengpiyan cave, one of the archaeological sites in Guilin City. The purpose of this work is to find out the structure characteristics of groundwater systems and identify migration pathways of the groundwater pollutants and their pollution sources. Combining the artificial sampling and highresolution online tracer technique and using sodium fluorescein and rhodamine B as the tracers, three tracer tests have been carried out around the study site. Based on these test results, the groundwater seepage field was analyzed and the average velocity of the groundwater was calculated. The results show that the flow velocity is about 1.6-33.91 m/d with anan average value of 12.92 m/d. The flow system in the karst area is basically dominated by a dissolution fracture network. There exists a northeastsouthwest trending main runoff zone; and it is unlikely to exist largescale karst channels that control the flow. The three tracer tests all indicate a hydraulic connection between the release points of pollutants and groundwater around the study site. Therefore, the localities such as residential areas, schools and previous brickyard can be identified as the pollutant sources which have a optional to pollute the groundwater in the relic cave. So it is necessary to expand the scope of protection of the relics, especially taking actions to prevent the leakage of the septic containers of the Zengpiyan scenic, which are now poorly closed and seriously harm to the environment of the relic cave.
Water geochemistry and runoff process of the Yiluochi karst water system
CHEN Xu, DU Yu-ben, JIANG Liang-wen
2016, 35(3): 254-261. doi: 10.11932/karst20160302
Abstract:
The Yiluochi karst water system lies in Longyang district, Baoshan City, Yunnan Province. It is on the western margin of the Baoshan basin. The primary aquifer of this system is composed of the sediment of O1y, which is bounded by the clastic rock and the fault. Geological structures with northwest and north-south trends dominate this region. The karst water system has a large karst spring with a flow rate of 440 L/s, as the main source of drinking water in Longyang district of Baoshan City. The proposed Baoshan tunnel of the Darui railway will cross the Yiluochi karst water area. This work has studied the formation of the karst water system and the characteristics of the groundwater flow, in order to provide a scientific basis for the design and construction schemes of the Baoshan tunnel, including the analysis of the influence of the tunnel project on the hydrogeological environment. The applications of chemical major elements and trace elements of the water and isotope analysis, in combination with regional water balance analysis, comprehensively permit to achieve the study objectives planned. The results of water chemistry analysis show the existence of a good correlation between the Yiluochi spring water and the stream water at Shahe river. The water samples of the Chaoyang village at Shahe river and Yiluochi exhibit a significantly higher SO42- content than the other water bodies, which also shows a relationship of the water between Shahe river and Yiluochi. The aluminium (as Al) anomalies of the water samples mostly occur in the water flowing through the Dabaogai syncline core area with the outcrop of O1l stratum, where the Al contents are merely 16.1 ug/L, which is similar to the content of samples from the upstream of the Shahe river. It proves that a little of the Yiluochi water is recharged by that from the syncline O1l stratum.Water balance analysis shows that O1y limestone accepts atmospheric precipitation as a recharge amounts up to 100×104 m3 per year, accounting for a small proportion of total water 1,387×104 m3 discharged via Yiluochi karst springs. It is believed that the Yiluochi springs are fissure water which flows along the limestone karst channels of the limestone interbeds in the Dabaogai syncline. The springs have no hydraulic connection with the upper bedrock fissure water. It is mainly developed in the O1y limestones of the Dabaogai syncline and feeds the Yiluochi springs. The main source of the spring water is the surface water from the upstream of the Shahe river near Chaoyang village, which is located in the northwest of the Dabaogai syncline.
Small catchment division in the typical karst landform areas:A case study of Jinsha county, Guizhou
CHEN Zhi-hu, YANG Guang-bin, YANG Chun-yan, ZHAO Lian-you
2016, 35(3): 262-268. doi: 10.11932/karst20160303
Abstract:
Prevention and control of soil and water loss and desertification in China are normally implemented on a small catchment as a unit basis. However, scientific study on the division of a small catchment in karst area has seldom been done. Jinsha county is located in a typical karst area in Guizhou, with various types of landform. This research was commenced on the work of digitization and DEM generation with the topographic map of Jinsha sheets on a scale of 1∶50,000. After that, the hydrological analysis module of GIS was used to automatically extract the small catchments, to merge the micro-catchments and in the meantime validate the basin boundaries from which 338 small catchments were finally extracted by the system. Result shows that the sizes of the small catchments fall in a range of between 3 km2 and 10 km2,accounting for 79.29% of the total small catchments. Within the range of integrity, and slope, and other three small catchment types, small catchment types in the study area is dominated by complete type of catchment. Most of the catchment boundaries can meet the requirements. In the areas with peak forest, peak cluster and karst depression, the boundaries do not exactly cross the top of the mountain or hill saddle. Due to the complexity of local drainage network, automatically extracted small catchments are not in accordance with the reality, which have to be manually modified.
Comparative study on nitrogen mineralization of soil in woodland and cropland in karst and clasolite regions
ZENG Si-man, LIU Man-qiang, CHEN Xiao-yun, ZHU Tong-bin, CAO Jian-hua, Christoph Müller
2016, 35(3): 269-273,281. doi: 10.11932/karst20160304
Abstract:
In this study, the 15N tracing technique and N transformation model were used to investigate the mineralization of labile organic nitrogen (as N) (MNrec), recalcitrant organic N (MNlab) and organic N (MNorg) to NH4+ in calcareous and red soils of woodland and cropland in karst and clasolite regions, respectively. The results show that soil N mineralization rates are significantly affected by soil types and land uses. MNorgin calcareous soil (3.71 mg N/kg/d) of woodland is considerably lower than that of red soil (5.57 mg N/kg/d). There is no significant difference between MNlab(1.81 mg N/kg/d) and MNrec(1.90 mg N/kg/d) observed in calcareous soil of woodland. However, the MNlab(4.60 mg N/kg/d) is much higher than MNrec(0.96 mg N/kg/d) in red soil of woodland. After converting woodland into cropland, the MNorglevel significantly increases to 4.21 mg N/kg/d in calcareous soil, but it decreases to 2.93 mg N/kg/d in red soil. In contrast to woodland, MNlabincreases by approximately 72.5% and MNrec decreases by approximately 33.7% in calcareous soil of cropland, respectively. CaO and MgO concentrations in calcareous soils are related positively with MNlab but negatively with MNrec, suggesting that soil CaO and MgO are the important factors affecting N mineralization rates in karst regions.
The effect of heavy rain event on soil temperature and soil volumetric water content in epikarst during summer
WU Xia, PAN Mou-cheng, ZHU Xiao-yan, BAI Xiao, ZHANG Bi-yun, ZHANG Mei-liang
2016, 35(3): 274-281. doi: 10.11932/karst20160305
Abstract:
To discover the carbon cycle in Guilin epikarst, the effect of heavy rain events on soil temperature and soil volumetric moisture has been studied. The HOBO equipment was used to monitor the the soil temperature and soil volumetric moisture content at depths of 20 cm and 70 cm in the summer of 2014 (July and August). The results shows a daily variation at the depth of 20 cm in soil temperature, which is mainly dominated by the daily variation atmosphere temperature. Soil temperature shows a steady increase at the depth of 70 cm, which is dominated by the increased atmospheric temperature due to summer monsoon. At the depth of 20 cm, soil temperature generally decreased and soil volumetric moisture content generally increased during and after the heavy rain events. At the depth of 70 cm, soil temperature increased first and then decreased, while soil volumetric moisture content increased during and after the heavy rain event. In the case of low soil moisture, the deep soil temperature can be elevated when the shallow high-temperature soil water infiltrates down. When the soil volumetric moisture content reaches a certain threshold, it can respond to storm events quickly. The results show that heavy rain events have different effects on soil temperature and soil volumetric moisture content at different depths in the karst area. Shallow soil can quickly respond to the heavy rain events, while the deep soil temperature and soil volumetric moisture content is not only dominated by the rain amount, but also by shallow soil temperature and soil volumetric moisture content.
An optimized fuzzy comprehensive evaluation model for assessment of soil heavy metal contamination in tea production parks of karst mountainous regions
SUN Xiao-tao, ZHOU Zhong-fa, HUANG Zhi-ling, CHEN Sheng-zi, ZHANG Shao-yun
2016, 35(3): 282-290. doi: 10.11932/karst20160306
Abstract:
An optimized fuzzy comprehensive evaluation model can facilitate to clarify the surface soil (0 ~ -20 cm) heavy metal contamination of tea producing park areas. Using Hg-Cd-Pb-Cr-Cu as evaluation factors and the principle of minimum relative information entropy, this study employed the "pollutant exceeding standard method" and "double weight method" to form a set of combined weight factors, which hence optimized the traditional fuzzy comprehensive evaluation model. Then we evaluated the soil heavy metal pollution in a tea producing park area and compared the evaluation results. We emphasize that the optimized evaluation model that integrates the soil heavy metal concentration and toxicity is much more suitable in the calculation of weights of evaluation factors and subsequent assessment result. The result shows that in the tea park area the soil clean ratio is up to 38.81% and moderately clean ratio is 61.19%. These data suggests that the overall soil environmental quality of this tea park area is fairly good, which meets the requirements of pollution-free tea production. Comparing the evaluation results shows that the optimized model is more scientific in grade classification, which can make the assessment more objective, and provide a reference for optimizing the layouts of tea production in karst mountainous regions.
Application of 3D electrical resistivity tomography to a tunnel in a karst area
ZHANG Xin, ZHAO Ming-jie, WANG Kui, RONG Yao, LIU Qiang
2016, 35(3): 291-298. doi: 10.11932/karst20160307
Abstract:
During the rainfall season the leakage of water in Nanshibi highway tunnel seriously influences the traffic of the tunnel, resulting in security risk. In order to find out the paths of leakage and sources of the water, this work used different devices of the high-resolution electrical resistivity to carry out in-situ measurements. Combining this survey with local geological conditions and other survey data available, the leakage situation of the tunnel was analyzed in detail. The results show that the high-density electrical method can work well by using different measurement devices and different running ways. In the Nanshibi tunnel, there are numerous karst cracks. The karst water mainly comes from the leakage of Meiling reservoir and supplement of rainfalls. Several major paths of the leakage have been clarified by the survey. This case study shows that the 3D imaging of electrical resistivity of the highresolution electrical method can reveal underground geological structure, which is of significance for detection and treatment of karst hazards.
Variations of cave water DICδ13C and its influencing factors in Furong cave, Chongqing
HUANG Chun-xia, LI Ting-yong, HAN Li-yin, LI Jun-yun, YUAN Na, WANG Hai-bo, ZHANG Tao-tao, ZHAO Xin, ZHOU Jing-li
2016, 35(3): 299-306. doi: 10.11932/karst20160308
Abstract:
To explore the variation characteristics of DICδ13C in the drip water and pool water in Furong cave, Chongqing, their influencing factors, and their impact on climate, the cave had been monitored from May 2013 to May 2014. The results showed that the CO2 concentration for both the soil air and cave air was high in summer and low in winter, which displayed significantly seasonal variations. They were affected by the combined effects of temperature and precipitation. The average DICδ13C value of the drip waters from five monitoring sites was -8.98‰, while the average DICδ13C value of the pool waters from two monitoring sites was -6.98‰, showing that the DICδ13C value of pool water was 2‰ heavier than that of the drip water. Corresponding to the arid climate in July 2013, the DICδ13C of cave water became heavier in October, while the light DICδ13C values indicated the delayed response to the humid climate. The DICδ13C of cave water showed a significant lag period to respond the climate change. The DICδ13C was dominantly affected by the soil CO2, also by bedrock dissolution, prior calcite precipitation and the opening degree of vadose zone. Our study demonstrates that on short time scales, the variations of DICδ13C of the drip water in Furong cave respond to the changes of local precipitation and the humidity conditions overlying the cave.
Source of cave CO2 and its spatial attributive characteristics of Zhijin Cave in Guizhou Province
ZHANG Shao-yun, ZHOU Zhong-fa, ZHANG Qiang, XIE Ya-ting
2016, 35(3): 307-313. doi: 10.11932/karst20160309
Abstract:
In order to explore the source of cave CO2 and its spatial distribution in karst plateau gorge area,a monitoring program on monthly basis was conducted at Zhijin Cave, Guizhou province, from January to July in 2015 for the monitoring of CO2 concentrations in cave and soil, cave water, soil moisture, rainfall and in the spring water above the cave. The results show that: (1) CO2 concentration in the soil above Zhijin cave is 11-17 times of atmospheric CO2, and 4-7 times of the cave CO2, respectively. The major sources of Zhijin cave CO2 come from air exchange and tourists respiration in horizontal direction; in vertical direction they are mainly from the respiration of plant root extending into the bedrock at the top of the cave, overlying cave foundation in karst fissure, soluble tubes entering inside the cave, the atmospheric CO2 ,and the freed CO2 due to the cave calcium carbonate deposition via groundwater degassing and dripping water in the cave. (2) Zhijin Cave is a multiline cave, the interpolation of space distribution of CO2 content showed characteristics of low ends and high in the middle, at the same time,the low value range of 800-1,000 ppm appears in the range of 1,200-1,400 ppm. In the whole cave, CO2 concentration tends to increase from both ends to the middle of the cave, along with an elevated altitude, which reaches a maximum value in Lingxiao Palace. (3) The groundwater in cave and soil water outside of the cave are both HCO3--Ca2+ type, while the atmospheric precipitation and spring water are SO42--Ca2+type.In the process of vertical migration, the chemical composition (hardness,Ca2+/Mg2+、HCO3-/SO42-、PCO2、SIc) in different parts of water from rain-spring-soil water-cave water is different.
Characteristics of physical and chemical properties and associated environmental implications of the karst water in Zhijin Cave of Guizhou Province
CAO Ming-da, ZHOU Zhong-fa, ZHANG Qiang, XIE Ya-ting, ZHANG Shao-yun
2016, 35(3): 314-321,348. doi: 10.11932/karst20160310
Abstract:
The aim of this work is to reveal the characteristics of dynamic changes of geochemistry and control factors of the cave water and their environmental implications. A dynamic monitoring over a period of 6 months from January 2015 to June 2015 was conducted for the water chemistry index of the Zhijin Cave in Guizhou Province. The results show that the water chemistry of this karst cave water is dominated by HCO3--Ca2+-Mg2+, where anion HCO3- is accounting for 84.5% and Ca2+and Mg2+are the dominant cations. The value of EC and concentrations of Ca2+, Mg2+,HCO3- and SO42- of cave drip water are higher than those of rock fissure water and pool water. The ratios of cave dripping water rate, drop volume, Ca2+, HCO3- and Ca2+/HCO3-have certain responses to climate. Their geochemical constituents have conspicuous seasonal effects. The EC value and Ca2+concentration of the cave dripping water have a notable linear relationship.
Review of research on element migration and environmental indicators in karst cave systems
LI Yuan, LIU Zi-qi, LV Xiao-xi
2016, 35(3): 322-331. doi: 10.11932/karst20160311
Abstract:
Using geologic carriers in cave systems to explore palaeoenvironment proxies has been conducted for many years. Elements in drip water and speleothem of cave as environment proxies are crucial in tracing their material sources, palaeoenvironments and palaeoclimate, which is commonly accepted by worldwide academics. Elements migration is mainly in the form of solution in karst cave systems, owing to dissolution and eluviation effects of rainwater on ground vegetation, soil and bedrock. It includes physical and chemical processes which control the element dissolution, migration and precipitation. It is an activation (dissolution)-migration (displacement)-combination (precipitation) reaction, which is influenced not only by climatic and environment (temperature, rainfall, CO2, etc.), but also by temporalspatial variation (migration path, residence time, etc.), while driven and restricted by CO2-H2O-CaCO3 circulation. Distinct differences exist in both element migration under different soil-rock conditions and element characters in the media of soil and bedrock, together with spatial heterogeneity of elements migration, all of which influence the material source of drip water and speleothem. Therefore, understanding the element sources of drip water and element migration mechanism in cave systems is a theoretical basis and premise for exploring element as environment proxies. This review is based on previous studies and outlines element migration mechanisms in karst cave systems. It focuses on systematical generalization of migration and variation mechanisms of Ca, Mg, Sr, and Ba in soil, bedrock and drip water. Sources and characters of each element are analyzed with environment impact factors. Then it summarizes the environment indicative significance which is reflected by element ratios in drip water and speleothem. Meanwhile,problems and prospects are pointed out for the research of element migration and environmental indicators in cave systems as follows,(1) Current explanation is unclear for the element migration in cave systems, because the migration process of karst water in cave roofs is complex and difficult to observe. So it is an emphasis in future study. (2) Cave drips and speleothem have diversities in their distribution coefficients due to the difference in time scales and media. In addition, environmental differences in study areas can lead to uncertainties and multiplicities in environmental indicator significances of element ratios. Here this review suggests to commence from environmental response mechanism of drip elements. Then we analyze the sensitive response changes of element proxies in drip water to different environments. Next we differentiate the material sources and response features of drip elements in different environments. Thus we can support speleothem research and enhance the accuracy of paleoclimate proxies. (3) We should commence from high-resolution rainfall response of cave drips and combine with surface environment features of rocky desertification. Then we extract sensitive indicators from drip water information of rainfall responses to reflect migration mechanisms of karst water, along with material sources of drip water. Thus we can establish an indicator system for underground monitoring under a rocky desertification environment, which provides scientific reference for the evolution process of the ecological environment with rocky desertification.
Research on evolution and dynamic mechanism of the ecological carrying capacity in karst rock mountain of southwest China :A case of Guizhou Province
YANG Ting-feng
2016, 35(3): 332-339. doi: 10.11932/karst20160312
Abstract:
The ecological sustainable development is an important condition for regional sustainable development. The status of the ecological carrying capacity and whether the ecological carrying capacity can support fast social and economic development have been important issues. In this article, Guizhou Province is taken as an example, to study the evolution and dynamic mechanism of the ecological carrying capacity by the calculation of carrying capacity based on ecological footprint theory. Data on each type of land use in Guizhou have been collected and calculated from 1978-2013. The results show that: the multi-year average total ecological carrying capacity is 2,690.560 ×104 hm2. From 1978 to 1986, the average total ecological carrying capacity is relatively low with the value of 2,440.734×104hm2; then from 1987 to 1989 the average total ecological carrying capacity shows steady improvement as a transition period; and from 1990 to 2013, the average total ecological carrying capacity reaches to 2,899.654×104 hm2. However, the ecological carrying capacity per capita in Guizhou shows a generally decreasing trend for many years with the multi-year average of 0.796 hm2. Among all land use types, ecological carrying capacity of cultivated land ranks the first, accounting for 65.9%,which is followed by woodland, accounting for 25.4%, construction land, accounting for 7.2%, pasture land, accounting for 1.4%, and water bodies, accounting for about 0.13%. From 1978 to 1985, Guizhou had ecological surplus, but decreased steadily. It changed to ecological loss from the beginning of 1986 and the situation has deteriorated each year. The evolution of ecological carrying capacity in Guizhou is mainly controlled by the type of land use, land productivity and population status.
Evaluation of urban landscape ecological security in karst areas based on 3S technologies:An example of Guiyang City
LI Xue-dong, YANG Guang-bin, ZHOU Yue, LI Bing, ZHANG Xu-ya
2016, 35(3): 340-348. doi: 10.11932/karst20160313
Abstract:
Accelerated urbanization and high-intensity exploitation of resources have brought serious impact on the natural ecosystem and the quality of urbanization. Previous studies on this issue focus on grasslands, watersheds, wetlands, and mountains, while the ecological vulnerable karst regions receive little attention. At the same time, the selected indicators are based on statistical data which ignore the spatial differentiation characteristics, which is not favorable to regional comparative studies and lacks visualization effects. Guiyang, the capital city of Guizhou Province, located in a typical karst region, is an ideal area for this research, because ecological environments, rocky desertification and severe degradation characterize in this city. Besides, the city lacks arable land and has high population pressure and extensive pattern of economic development, forcing the urbanization process to accelerate and in turn increase the urban ecological security threat. This study is based on the theory of landscape ecology, using the "pressure-state-response (PSR)" model to build an urban landscape ecological security evaluation system of karst areas. The evaluation indexes include population pressure, urban sprawl, vegetation fractional coverage, the degree of rocky desertification, habitat quality index, urban heat-island effect and natural hazards. By comparing and analyzing the spatial distribution and evolution characteristics using multi-temporal of remote sensing data and GIS technology, this work obtains urban ecological security levels distribution in 2000 and 2013 for Guiyang City. The results show that the ecological security index of Guiyang City was relatively low in 2000 and 2013, with 3.04 more than the level of security in 2000 and 1.78 in 2013. In terms of spatial distribution, the security index tended to increase from southwest to northeast . The variation map of urban ecological security between 2000 to 2013 is obtained via superposition analysis by ArcGIS, in which the ecological security change area accounted for 27.89% of the total. The extremely strong degradation area is 0.15%, strong degradation area is 2.58% and the degradation area 20.10%; and the optimization area and strong optimization area are 4.55% and 0.46%, respectively. Moreover, classification of landscape types is done using the object-oriented method in the research. Next, this work overlays the classification results and urban ecological security data, and makes statistics to the values of ecological security at different landscape type. The results show that the ecological security of landscape types mainly concentrate at unsafe, critical, and secure levels. The urban areas mostly fall in a ill-conditioned level. With the increase of security levels, the proportion of occupying areas reduces gradually. The farmland landscape above in the safe level decreases and increases at other levels to some degree, but the overall trend is not obvious. The change trends of ecological security are roughly same in grasslands, forests and shrub landscapes. Wetland landscape type ecological security level is improved markedly. Comparing the ecological security of landscape types between 2000 and 2013, we find the ecological security indexes of all the landscape types tend to significantly decline except for wetlands. Degradation of farmland is more obvious and the wetland is the only improved landscape type. During the research period, landscape ecological security situation in Guiyang City indicates a trend of deteriorating. Therefore it suggests to optimize land use pattern in urban planning and construction in the future in order to raise the urban landscape ecological security level.