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2020 Vol. 39, No. 2

Display Method:
Evaluation status and problems of groundwater resource potential in Yunnan Province
WANG Yu
2020, 39(2): 137-146. doi: 10.11932/karst20200201
Abstract:
Yunnan Province is located in the southwest of China,bordering Vietnam,Laos and Myanmar,with a total area of 394,000 km2. The mountainous area of Yunnan Province accounts for about 94% of the total land area.The terrain is high in the northwest and low in the southeast,descending in a ladder form from north to south.The highest point is the Kawagbo peak of Meili snow mountains at the border between Yunnan and Tibet,with an altitude of 6,740 m.The lowest point is at the intersection of the Nanxi river and Honghe river in Hekou county,with an altitude of 76.4 m.The distance between the two points is about 900 km as the crow flies,with height difference over 6,000 m.The general topography of Yunnan is bounded by the Yuanjiang and Yunling mountains,which are divided into two parts.The eastern part is the central Yunnan red bed and the eastern Yunnan karst plateau,with an average elevation of about 2,000 m.Here landform is gentle rolling mountains,low mountains and hills,among which karst faulted basins are prevail.The western part is the longitudinal valley of the Hengduan mountains,with an elevation of about 3,000-4,000 m.It consists of the Gaoligong mountains,Nu mountains and Yunling mountains and the Nu river,Lancang river and Jinsha river,forming a "Three parallel rivers" landform wonder.In the south,the Hengduan mountains and valleys are remaining,with gentle terrain in general,and the river valley is gradually broad. In the border areas in the south and southwest,the terrain is low and gentle,hosting many wide valley basins,generally about 800-1,000 m above sea level,and some sections are lower than 500 m.Yunnan has generally a subtropical plateau monsoon climate,with distinct dry and rainy seasons.Due to the specific geographical conditions,the formation of water resources in space and time distribution is uneven,resulting frequent drought in winter and spring.Regional hydrogeological surveys show that the average runoff of groundwater in the province is 74.274 billion m3?a-1,and the allowable yield of groundwater is about 19.035 billion m3?a-1.Groundwater resources have the characteristics of wide distribution,stable dynamics and excellent water quality,which play an irreplaceable role in daily and drought-resistant water supply.Groundwater resource potential refers to the amount of the allowable yield of groundwater that can be available for expansion under the condition of groundwater exploitation and utilization.The specific value is,the difference between the amount of allowable yield of groundwater resources in the evaluation area or aquifer and the amount of actual exploitation.The purpose of this paper is to accurately evaluate groundwater resource potential in Yunnan Province for the development and utilization of groundwater resources including science planning,protection and management,and provide guidance,in-depth investigation,and evaluation.Our analysis builds on the system science theory,historical analysis,the principle and method of hydrogeology and water balance analysis,abundant groundwater resources investigation data,and dynamic monitoring data.We evaluate and analyze the development and problems of groundwater resources potential in Yunnan Province.In a systematic investigation of the history and present situation,the groundwater resource potential evaluation methods and results are reviewed.The utilization rate of groundwater resources is 30.32%-51.49% in intermountain basins where the cities above country level are located,and that in the vast mountainous area is 9.63%-30.0%.The current status quo of groundwater resource potential is about 13.448 billion m3?a-1.At present,the basic hydrogeological survey is in the general survey stage,and there are still large gaps in the northwest and west Yunnan,so the evaluation results of the provincial and regional groundwater resource potential only reach the accuracy of inference and prediction. For the first time, the main problems are analyzed systematically,such as poor understanding of water resources and the environmental system,incomplete evaluation contents and standards,and insufficient monitoring and forecasting of water quality and water quantity,which lays a good foundation for a new round of water resources investigation and evaluation.
Numerical study on surface water leakage replenishment of the Fenhe 2nd reservoir into the Jinci spring system
LIANG Tengfei, CHENG Jianmei, ZHANG Naiyan, SHI Wen, KAISAERJIANG·Aihemaiti
2020, 39(2): 147-153. doi: 10.11932/karst2020022
Abstract:
Due to the construction of the Fenhe 2nd Reservoir, some essential conditions about surface water leakage into karst groundwater system have changed in the Jinci spring area, which affects the regional karst water flow field changes in future. In this study, based upon systematic analysis of formation lithology and water level in the Fenhe 2nd Reservoir area, the contribution of reservoir leakage to the Jinci spring has been determined. Then, a three-dimensional groundwater flow model has been built to investigate the impacts of reservoir leakage into karst groundwater flow system, and the groundwater level change trend at outlet of the Jinci spring is predicted when the Fenhe 2nd reservoir runs in the different scenarios. The results showed that, the leakage into the Jinci spring area increases with the rise of the reservoir water level, and its proportion changes non-linearly, which lowest is 92.8% and stabilizes at 93.7% after water level reaches 902 m.The groundwater level rise is mainly affected by the recharge distance from the leakage zone. The runoff zone of Jinci spring karst water system is most significantly affected by reservoir leakage, followed by the discharge area and the northern recharge area. Besides, it is concluded that, the groundwater level near the Jinci spring can reach to its spring outlet elevation by July,2021 and January,2023 when the reservoir water level stays at designed level of 905.7 m and the level in 2017, respectively.
Flow recession analysis of karst underground river basins in different karst geomorphic units in the upper reaches of the south source of the Wujiang river, Guizhou Province
GONG Xiaoyu, ZENG Cheng, HE Chun, CHEN Wangguang
2020, 39(2): 154-163. doi: 10.11932/karst2020y22
Abstract:
The Sanchahe river basin is located in the transition zone from the Yunnan plateau to the Guizhou Plateau, which is the south tributary of the Wujiang river. The total area of the basin is 7,264 km2, where elevation drops from 2,000 m to 1,100 m. This basin hosts many multi-phase karst and diverse landforms. Within this basin, the Huayudong sub-underground river basin and the Santang sub-underground river basin are located in the karst peak-cluster region of Panxian-Weining and the karst peak forest region of central-southwest Guizhou, respectively, possessing different karst development characteristics. To investigate the relationship between karst surface morphology and structure of karst water-bearing medium, this work uses the topographic indexes (elevation and relief) of the two basins to compare and analyze their geomorphologic development features, and determine structural characteristics of the water bearing medium in the two basins by the flow recession analysis based on interval exponential function. Results show that, (1) The Huayudong underground river basin has an average elevation of 2,306 m and an average relief of 73.2 m. It can be divided into two areas: high relief area I (mean 122 m) and low relief area II (mean 64 m), which account for 14.9% and 85.1% of the whole basin area, respectively. The Santang underground river basin has an average elevation of 1,880 m and an average relief of 87.6 m. It can be divided into three areas: high relief area I (mean 106 m), medium relief area II (mean 81 m)and low relief area III(mean 48 m),which account for 40.2%, 49.7% and 10.1% of the whole basin area, respectively. (2)The recession coefficients of each stage of the Huayudong underground river basin are 0.000,3, 0.000,1, 0.000,06 (1/0.5 hour), the total water storage capacity is 2,199.356×104 m3, and the water storage of different hydrological sub-regime accounts for 0.1%, 9.9% and 90.0% of the total water storage, respectively. The recession coefficients of every stage of the Santang underground river basin are 0.001, 0.000,3 and 0.000,1 (1/0.5 hour),the total water storage capacity is 2,310.902×104 m3, and the water storage of different hydrological sub-regime accounts for 9.4%, 30.8% and 59.8%, respectively. These results suggest that there may be some correlation between surface relief and flow recession, that is, high relief corresponds to strong karst pipeline flow (the first flow recession state), and low relief corresponds to aquifers (the second and third flow recession state) with small fissures and karst cracks.
Sources and transformation of nitrate in karst groundwater of Zengpiyan site, Guilin
WU Xisong, ZHANG Qiang, JIANG Guanghui, GUO Fang, WU Huaying, LUO Junhui
2020, 39(2): 164-172. doi: 10.11932/karst20200202
Abstract:
The peak-forest plain is a concentration area of human activities and living, and also the main runoff and discharge section of karst groundwater systems, with rich groundwater resources. With the development of urbanization, the problem of groundwater nitrate pollution has becomes increasingly prominent. In order to study the source and transformation of nitrate in the karst groundwater of Zengpiyan site in Guilin, groundwater samples were collected in October 2018, February 2019, March 2019 and April 2019, respectively.By virtue of these samples, using conventional water chemistry and nitrogen and oxygen isotope techniques, this work identified groundwater nitrate sources and transformation process. The results show that the concentration of NO3- in the groundwater of Zengpiyan is 0-19.523 mg?L-1, and δ15N-NO3- and δ18O-NO3- are between -0.17 ‰-45.12 ‰ and -5.82 ‰-16.47 ‰, respectively. According to the data of nitrogen and oxygen isotopes of groundwater in the study area, the source of nitrate in groundwater is mainly feces and wastewater, a small amount of nitrate comes from NH4+ in rainfall and soil organic nitrogen. Controlled by the heterogeneity of karst medium, NO3-concentration, δ15N-NO3- and δ18O-NO3- in the groundwater of Zengpiyan show obvious spatial variability. The process of nitrate transformation of groundwater in Zengpiyan is complex, which is controlled by seasons and the heterogeneity of karst medium. Denitrification is the main process in dry seasons and nitrification in rainy seasons. Clarifying the source and transformation of nitrate can provide a scientific basis for the control of nitrate pollution in groundwater of the Zengpiyan site.
An experimental stuty on in-situ nitrate-contaminated remediation of karst water
YE Jinxia, XIA Chunying, BU Hongzhi
2020, 39(2): 173-179. doi: 10.11932/karst20200203
Abstract:
The extremely inhomogeneous nature of karst aquifers make the cyclic movement of karst water controlled by structure, fissure space and development direction. Due to the complex environmental conditions, it is difficult to carry out in-situ remediation of karst water pollution. Up to now, there is no report on this issue in China. This work chose the typical karst development and nitrate-contaminated areas in central and southern mountainous area of Shandong province to construct a pilot project by drilling holes. The in-situ nitrate-contaminated karst water remediation tests were carried out by using the approach of“ethanol + glucose” liquid carbon source and the “polyvinyl alcohol + starch granule” solid-state reactor. The results show that: (1) the degradation rates of nitrate concentration in the denitrification solution of “ethanol + glucose” with concentration of 500 mg?L-1 and 1,000 mg?L-1 are 6.45% and 21.52%, respectively. (2)When denitrifying solid-state reactor of “polyvinyl alcohol 3 kg + starch granule 3 kg” and “polyvinyl alcohol 2 kg + starch granule 4 kg” with unit length component materials was used to denitrify the nitrate concentration, the degradation rates are 33.91% and 34.96%, respectively. The test proves that it is feasible and effective to adopt the in-situ remediation technology of groundwater pollution by using the hole group scheme in karst areas, which can achieve remarkable results. The layout of the remediation project and the test results of this work have certain reference significance for the in-situ remediation of karst groundwater pollution in similar areas.
Analysis on water use efficiency of plants at different altitudes in karst graben basin
LIANG Jintao, DENG Yan, LI Xuyao, XU Ye, CAO Jianhua
2020, 39(2): 180-188. doi: 10.11932/karst20200206
Abstract:
The Xiaojiang river watershed is a typical karst graben basin in the edge of the karst plateau and valley slopes in eastern Yunnan. The basin spreads from northeast to east, with terrain overall high in the north and east and low in the south and west. The geomorphology within the basin is divided into five types,karst platform trough valley in the upstream, karst mid-mountains surrounding the basin,basin-level sedimentary flats, karst peak-cluster depressions around the basin bottom, and Xiaojiang karst valley. The basin is located on a low-dimensional plateau, has a sub-tropical and semi-humid climate,a characteristics of the central Yunnan plateau.It hosts different vegetation types associated with the influences of the topography and geomorphology on the distribution and reconfiguration of water,heat, and soil conditions. This study attempted to explore the relationship between nutrients, environmental factors and plant water use efficiency changes at different altitudes,focusing on the trees, shrubs, and herbs in the basin. The stable isotope 13C was used to calculate water use efficiency.Water Uuse Eefficiency (WUE) and leaf nutrient concentration with the altitude were analyzed.The research shows that, (1) in the study area, the δ13C value of the herbaceous plants at 2,000 m is the highest, and the δ13C value of the tree leaves at 2,200 m is the lowest. (2) The tendency of WUE changes at different altitudes is variable,and the effect of altitude on the water efficiency of trees and shrubs is greater than that of herbaceous plants.The water efficiency of herbaceous plants varies little with altitude, and the fit degree between them is small.The high value area appears in the trees at an elevation of 2,200 m, the low value area appears in the herbs at the elevation of 2,000 m. (3) The correlation between WUE and leaf N and P concentrations is weak at different altitudes.WUE is weakly positively correlated with leaf N concentration, and weakly negatively correlated with leaf P concentration. (4) The correlation between WUE and various climatic factors at different altitudes is weak.The elevation WUE is positively correlated with the average annual temperature, the average annual rainfall,and the average annual sunshine hours.It is noted that the correlation between WUE and other environmental factors is not significant,which is a comprehensive manifestation of the special spatial heterogeneity of the coexistence of "basins and mountains" in the graben area.
Effects of agricultural cultivation on soil organic nitrogen mineralization in karst regions
WEN Dongni, YANG Cheng, YANG Lin, QIN Xinghua, MENG Lei, HE Qiuxiang, ZHU Tongbin, Christoph Müller
2020, 39(2): 189-195. doi: 10.11932/karst20200207
Abstract:
The mineralization of organic N dominates the production of inorganic N, therefore, it is of great significance to study the change of soil N availability and to guide N fertilization. Soil samples under navel orange, corn and rubber plantations were collected in karst regions of Jianshui,Mengzi and Mengla, Yunnan Province, respectively, and the adjacent undisturbed grassland and natural forest were sampled as control. The 15N tracing technique was used to investigate the changes in the mineralization rate of organic N to NH〖_4^+〗 (MNorg) in calcareous soil when grassland or natural forest was converted to croplands in karst regions, and the contributions of the mineralization of labile organic N (MNlab) and recalcitrant organic N (MNrec) to MNorg were quantified. The results showed that MNorg rate in forest soils (8.94 mg N?kg-1 d-1) was significantly higher than that in grassland soils (1.41-2.46 mg N?kg-1 d-1). Soil MNlab dominated MNorg, accounting for 80.6%-93.1% of MNorg in grassland soils and 62.2% in forest soils, respectively. Soil MNorg was significantly reduced to 0.53-0.89 mg N?kg-1 d-1 during the conversion of grassland or forest to cropland, with a decreased ratio of 62.5%-90.1%. When grassland was converted to navel orange or corn plantations, MNlab rather than MNrec was responsible for the decreased MNorg. However, the decreased MNorg was mainly attributed to the simultaneous decline in MNlab and MNrec when natural forest was converted to rubber plantation. The contents of soil organic carbon, total N, total phosphorus, total calcium and total magnesium, as well as pH, CEC and WHC were significantly reduced during the conversion of grassland or natural forest to cropland in karst regions, all of which were positively correlated with soil MNorg and MNlab, indicating that the changes in soil physical and chemical properties during agricultural cultivation was an important factor affecting MNorg.
Spatiotemporal variation of vegetation coverage in plateau mountainous areas based on remote sensing cloud computing platform: A case study of Guizhou Province
WU Yue, ZHOU Zhongfa, ZHAO Xin, DAN Yusheng, HUANG Denghong
2020, 39(2): 196-205. doi: 10.11932/karst2020y16
Abstract:
The purpose of this work is to reveal the spatio-temporal variation of vegetation in karst mountainous areas. We choose the Landsat-NDVI images of 1748 scenes with 30 m resolution during 2000-2018, combined with data from 35 meteorological stations and the pixel dichotomy model, linear trend analysis and geographic detectors to quantitatively estimate the annual vegetation coverage in Guizhou Province in the past 19 years. The spatial and temporal variation and driving forces of vegetation coverage were analyzed. The results show that,(1) the areas of medium-high vegetation coverage account for 63% and the area of high vegetation coverage accounts for 21.16%, which is mainly concentrated in the clastic areas. On the whole, the amount of vegetation coverage is of such an order: clastic rock > dolomite > limestone. (2) In the past 19 years, the vegetation coverage in Guizhou Province has shown slight improvement, with an average annual growth rate of 0.4%. The multi-year average value of maximum vegetation coverage in severe rocky desertification areas is constantly lower than the general vegetation coverage. (3) During the study period, the overall change of vegetation coverage in Guizhou Province was stable, dominated by slight improvement and basically no-change, the sum of which accounts for about 95.4% of the total area. The degraded areas are mainly distributed in periphery of cities and towns, accounting for about 3.8% of the total area. (4) The interaction between meteorological and geographical factors has greater impact on the spatial pattern of vegetation coverage than that of single factor. In summary, the key factors affecting vegetation restoration and ecological environment reconstruction include urban area expansion, rocky desertification control project, geographical location and meteorological factors. The study of multi-year dynamic characteristics of vegetation coverage aims to provide important basic data and scientific reference for water and soil conservation, ecological environment protection decision-making, ecological restoration (rocky desertification control) and sustainable management of relevant departments.
Characterization of karst paleo-geomorphology and the paleo-water system on the top of the 4th member of the Dengying formation in the Gaoshiti area, Sichuan basin
LIU Xixiang, DAN Yong, LUO Wenjun, LIANG Bin, XU Liang, NIE Guoquan, JI Shaocong
2020, 39(2): 206-214. doi: 10.11932/karst20200210
Abstract:
Karst pore-cave reservoirs of the Dengying formation developed well in the Weiyuan, Ziyang and Gaoshiti-Moxi areas in the Sichuan basin, which are heterogeneous, thus making reservoir prediction difficult. One of possible approaches to solve this problem is recover the karst paleo-geomorphology and paleo-water system from the karst geological theory, so as to reveal the development and distribution of the reservoirs to guide exploration. In this paper, the karst paleotopography in the Gaoshiti area is restored by the impression method. Combined with the modern karst and karst dynamics theory, paleogeomorphology (second-class)are divided unto three types of the third class:karst platform, karst gentle slope and karst basin. Based on the modern karst classification method, according to the micro-geomorphic combination form, the second-class paleogeomorphology is finely characterized, and six kinds of third-class paleogeomorphology units are divided. Finally, according to karst dynamics and karst hydrogeology, The three major water systems, i.e. the north, west and southeast are depicted in the Gaoshiti area. It is considered that different geomorphological locations have different hydrodynamic conditions, and there are differences in the developmental characteristics of different types of karst paleogeomorphology, runoffs in ancient water systems, excretion and reservoir development, and filling characteristics. The fine paleogeomorphology and the depiction of the ancient water system have great importance for advancing oil and gas exploration and development of the Dengying formation in the Gaoshiti area.
Tectono-sedimentary differentiation of lower Palaeozoic carbonate rock in Ordos basin, NW China and its implications for hydrocarbon-play generation
ZHANG Xiaoxing, CHEN Anqing, DANG Niu, ZHANG Chengong, ZHAO Junxing, GAO Xing, LAN Yefang, CHEN Hongde
2020, 39(2): 215-224. doi: 10.11932/karst20200211
Abstract:
The Lower Paleozoic carbonate rock in Ordos Basin is a major target of oil and gas exploration. At present, the potential reservoirs and traps of this rock in different tectonic units of Ordos Basin remain not well understood, which hinders prediction of preferable exploration targets. To solve this problem, based on the analysis of sedimentary and tectonic features, this paper reveals the sedimentary evolution and structural transformation of early Paleozoic carbonate rocks in the Ordos Basin. The results show that controlled by the Central ancient uplift and the epeiric sea environment, the southern margin of the basin is characterized by the development of rimmed reef-shoal facies association, the western margin is characterized by the development of bedded reef-shoal facies association, and the intracratonic basin is characterized by tidal flat of limited platform.The carbonate formations in the three different facies belts have favorable conditions for hydrocarbon-play generation, but their tectonic transformations are significantly different, which can be divided into a compressive tectonic unit in the west margin, extensional tectonic unit in the south margin and stable tectonic unit in the inner craton. Favorable traps in the broken fold belt of the western intracontinental foreland basin include overthrust faulting traps and secondary anticlinal traps in syncline. Traps related to buried hills developed in the south extensional tectonic unit affected by the Weibei graben. The Yishan slope of inner craton is a large monoclinal structure with weak reformation and lots of lithologic traps, and the macroscopic distribution of those lithologic traps are mainly controlled by rotary tidal current of the epeiric sea.
Process and influencing factors of karst ground collapse in the water source area of Tai’an-Jiuxian
WU Yanan
2020, 39(2): 225-231. doi: 10.11932/karst2020y23
Abstract:
Tai’an City lies in the western margin of the Tailai basin in Shandong Province, where karst is pervasive and controlled by regional geological setting. The karst collapse in this area started in the 1960s, causing serious social-economic impacts. This geologic hazard is a complex and multi-factor process, occurring mainly in the central and southern Tai’an City with high intensity of groundwater exploitation. The affected regions include, (1) the urban subsidence area, centered at the triangle south of Tai’an railway station with east boundary to the Shanggao street office south boundary to Honggou village, where limestone is widely present in the subsurface. (2) The Jiuxian subsidence area, which is centered at the Jiuxian water source area southeast of the city. (3) The Yanglou subsidence area, with east and west Yanglou village as the center, actually the periphery of the Jiuxian subsidence area. These three regions are largely connected into one, forming a karst collapse belt from the Jiuxian village to Taishan railway station, with an total area of about 200 km2.The objective of this work is to reveal the historical process and influencing factors of karst collapse in the study area,so as to provide the scientific guidance for prevention and control of this geologic hazard.We firstly summarized the initiation and development process of karst collapse in the study area.Then, based on the previous research results and the latest surveys,we analyze the distribution of the hazard and its basic control factors, as well as the action laws and mechanisms of each factor.The results show that the influencing factors of karst collapse can be divided into natural and human factors.(1) Under natural factors,karst collapse mainly occurs in the areas with intense karst development, near fault zones, and soil layer thickness less than 30 m. The Quaternary soil structure is mainly a binary-layer structure, followed by a multi-layer structure; most of the collapses occurred in the flood season, especially after heavy rainfall.(2) Under human factors,the large water level fluctuation caused by strong groundwater mining is the most important factor for the occurrence of collapse;and the fluctuation of karst groundwater level near the bedrock surface is the most likely to cause the collapse.Moreover,the karst collapse in the Jiuzhen railway interchange area is also closely related to the train vibration. Finally,some suggestions are put forward in this paper, the future research should be focused on the monitoring and simulation of collapse evolution, exploration of collapse forecasting methods , and the construction of database .
Response characteristics of karst groundwater to rainstorm and the multiple regression prediction model in Dachengqiao, Ningxiang county, Hunan Province
PAN Zongyuan, WU Yuanbin, JIA Long, YIN Renchao, MA Xiao, CHEN Ting
2020, 39(2): 232-242. doi: 10.11932/karst2020y12
Abstract:
The groundwater activity in the karst mining area can cause serious geological hazards. It is the key to solve the problem of frequent disastersto understand the response characteristics of groundwater to extreme climate conditions. The Dachengqiao area was selected as the study area, which is about 2 km away from the Meitanba coal mine.The stratigraphic lithology in Dachengqiao is mainly the calcareous conglomerate of Cretaceous Baihuating formation, followed by limestone of Permian Qixia formation and Maokou formation.Affecting by the mining drainage karst aquifer,the maximum water level of Dachengqiao is more than 90 m deep.The main runoff direction of groundwater flows from south to north, and is discharged to the mine. In this paper,through the on-site monitoring methods such as the high frequency monitoring of karst groundwater level and rainfall,the dynamics of karst groundwater level and itsresponse process to heavy rainfall are studied,and the characteristics of ground water internal relationship are discussed and a regression predition model is established. The results indicated that karst groundwater level responded quicker to rainfall in rainy season, and the amplitude of groundwater level is larger compared with that in the dry season. Under the rainstorm condition, the dynamic response of karst groundwater level to the rapid pipeline flow is a steep rise-steepfall,with the variation range of 13.6 to 42.8 m.Whereas the dynamic characteristics of groundwater level supplied by fracture and pore water are slow rise-slow fall,withan annual variation of 1.1 m. The lag time of groundwater level response to rainstrom in therainy season ranged from 1.2 to 4 h, which is 1/2 to 2/3 shorter than that under the same conditions,and groundwater level variation increased by 1.7 to 4.7 times. In dry season,the lagtime of groundwater level response to rainstorm ranged from 4.2 to 13.2 h, which is extended by 3 to 8 h, and groundwater level variation is reduced by 5 to 11 times. According to the research, groundwater level dynamic characteristic was controlled by thickness and water saturation of vadose zone, which indicated thickness of vadose zone presented a negative relationship with response lag of groundwater level, and water saturation of aeration zone presented a positive relationship with groundwater level variation. The optimum regression prediction model is established through correlation analysis, fitting optimization, variance and residual analysis, and regression coefficientt test, which indicates as Hi=14.149+0.308y1+0.379y2-0.023Pi+0.051Ti. It is proved that the model can effectively predict the water level change process of monitoring sites under the condition of rainstorm.
Application of pressure water tests to evaluation of grouting effects on the karst roadbed
FENG Haiming
2020, 39(2): 243-250. doi: 10.11932/karst20200214
Abstract:
Karst is common in the area where the Guizhou-Zhangzhou-Changzhou railway passes through, of which landforms are characterized by depressions, sinkholes, caves and cracks. The roadbeds in this area are mostly susceptible to collapse as shown by regional geological evaluation. The consistency of evaluation of grouting effects is a difficult issue. At present, there are many methods to evaluate the effect of karst treatment, which, however, are mainly qualitative. This work aims to explore a quantitative method by pressure water tests to evaluate the grouting effect in karst areas. Firstly, various evaluation methods are presented. Then feasibility of quantitative evaluation of grouting by pressure water tests is analyzed. A representative section of grouting tests at the karst roadbed of the Qianjiang-Changde railway is selected as an example and the different cases with four kinds of qualified criteria are examined, indicating that the current qualification criteria have some advantages and disadvantages. Combined with theoretical analysis and practical application, a new criterion for quantitative evaluation of the grouting effect is established on the basis of many tests and optimization schemes. And the technological parameters of the pressure water test are summarized. The pressure water test method used in this work is a single-point method, in which the number of the pressure water tests before and after grouting is no less than 5% and 4%, respectively; the test pressure is 0.05-0.25 MPa, the test length is 3-6 m, and the pressure water time is 5-10 minutes per time. The results show that the new evaluation criterion verified by 44 sections of water pressure tests is more reasonable and accurate than the other single criteria. Meanwhile, the fuzzy evaluation of drilling, and geophysical prospecting is used to verify the criterion again, which suggests that the criterion is basically consistent with other evaluation results, showing good applicability and rationality. In all, this criterion is a suitable and reliable method for quantitative evaluation the grouting effect on the karst roadbed.
Development characteristics and research value of red carbonate stone forest in the Xiangxi geopark
WU Liangjun, CHEN Weihai, RONG Yuebing, ZHANG Jing, HUANG Chao, ZHU Haiyan, MENG Qingxin, WU Jiwen, LUO Qukan, BAI Bing, OU Mengmeng
2020, 39(2): 251-258. doi: 10.11932/karst20200215
Abstract:
The red carbonate stone forest is one of the most important geologic relics in the Xiangxi geopark. This forest formed in Ordovician Dawan Formation and Guniutan Formation, concentrated in the canyon-slope area along the Youshui-Mengdong river. Its exposed area is about 84 km2, and can be regarded as the largest known Ordovician red carbonate stone forest landscape in the world. The red stone forest has various forms and good landscapes, including astower, flame, wall, sword, column, and andcone. In geological genesis, similar to the other karst stone forests, the formation of the red stone experienced stages of stratigraphic sedimentation, tectonic uplift and weathering erosion. The suitable palaeogeographic environment, fissure morphology, tectonic uplift, warm climate and abundant surface and underground water systems are the major conditions for the development of the red stone forest. However, due to some special factors, such as complex lithological composition, thin strata and different dissolution, the red stone forest has obvious superposition shape of vertical and horizontal dissolution marks, with unique natural beauty,which is quite different from some other well-known stone forests, for example the Yunnan stone forest and Xingwen stone forest. This phenomenon might be attributed to a unique process of formation. In colour, the red stone forest shows amazing changes in different kinds of weather and different times of the year,which may be caused by algae on the surface of the pillars. Besides the southwest of China, the distribution of Ordovician red carbonate stone forests is very limited, only reported of Satun of Thailand with prominent rarity. Just due to the scarcity, many targeted studies remain in infancy, which is worthy of further in-depth research by scholars of various disciplines.
A prediction method of karst cave scale based on the binary classification model of the Gaussian process
ZHANG Binghui, ZHANG Yan, WANG Wei, LIANG Jiahao
2020, 39(2): 259-263. doi: 10.11932/karst2020y04
Abstract:
A complex non-linear relationship exists between the scale of karst caves and its influencing factors. While the scale of karst caves can be predicted by pattern recognition based on influencing factors. A method based on the Gaussian process for the binary classification model (GPC) is proposed to predict the scale of karst caves. In this method, the complex nonlinear relationship between the scale of karst caves and influencing factors is established by learning a few samples. It gives probabilistic output identification for forecasting samples that only provide influencing factors. Research suggests that the proposed method not only has merits of small training samples, self-adaptive parameters determination and high recognition accuracy, but also can give the probabilistic credibility for prediction results. This method can provide a quantitative basis for effective prediction of the scale of karst caves in engineering practice, and has a good application prospect.
Characteristics of culturable bacterial communities in karst caves with different CO2 concentrations: An example of the Xueyu cave and Shuiming cave in Chongqing
CHEN Jiyu, LU Zujun, HE Qiufang, LI Qiang
2020, 39(2): 264-274. doi: 10.11932/karst2020y20
Abstract:
Despite many reports on the excavation of bacterial resources in caves. There is still no detailed report on how the culturable bacteria in caves respond to different concentrations of environmental factors (especially CO2 concentration).The purpose of this work was to examine the community characteristics of culturable bacteria in karst caves with different CO2 concentrations and reveal the response of culturable bacteria to relevant geochemical indicators.In 2018,sediment and rock wall samples of karst caves were collected from the Xueyu cave and Shuiming cave with different CO2 concentrations in Chongqing.The gas collection bag was used to collect gas in the caves to measure CO2 concentration. Water samples from the surface of the sediments in the two holes were collected and packed in polyethylene plastic bottles for the determination of HCO〖_3^-〗.The rock wall and sediments of the two caves and water bodies were collected and packed in sterile bags for culture and geochemical index determination.Four kinds of isolation media were used to enrich and culture different types of bacteria,and phylogenetic analysis was carried out.The 16S rRNA gene sequence was amplified by PCR using 27F/1492r as the forward and reverse primers (27F:AGAGTTTGATCCTGGCT;1492r:GGTTACCTTGTTACGACTT).The amplification conditions were pre denaturation at 95 ℃ for 5 min, denaturation at 94 ℃ for 30 s, annealing at 52 ℃ for 30 s, extension at 72 ℃ for 1.5 min,35 cycles,extension at 72 ℃ for 10 min,and preservation at 12 ℃,respectively.Cluster x software was used for multiple sequence alignment, and the phylogenetic tree was constructed by MEGA5.0, and SPSS 25 software and Pearson correlation coefficient method were used to analyze the correlation between geochemical parameters and dominant OTUs.The results are as follows,(1) The abundance of culturable bacteria in the Shuiming cave is significantly higher than that in Xueyu cave.(2) Based on 16S rRNA gene sequence analysis, 244 strains of bacteria are isolated and purified, which belong to 87 different OTUs. Culturable bacteria are mainly composed of Proteobacteria, Actinobacteria, Firmicutes, Bacteroidetes and Deinococcus-Thermus. Bacteroidetes only exist in the Xueyu cave with high CO2 concentration, then it is speculated that Bacteroidetes can tolerate high CO2 concentration.(3) CO2 concentration is one of the important factors that affect the bacterial abundance, community and activity in karst caves. It is speculated that the negative δ13C-CO2 values of the Xueyu cave and Shuiming cave may be the result of the interaction between microorganisms and hydrogeochemistry. These results suggest that high CO2 concentration inhibit most microbial abundance and diversity. The high concentration of CO2 may be attributed to reduction of the pH inside and outside the cells affecting the metabolic activity of bacteria and the bacterial enzyme system. However, some special cases exist, for example, the relative abundance of Bacteroides increases from 3.09% to 21.20% with the increase of CO2 leakage. The respiration and hydrogeochemistry of overlying soil can lead to the negative value of δ13C-CO2 in caves.
Self-purification ability of tourist caves on a short-term scale: An example of the Dafeng cave in Suiyang county
FAN Baoxiang, ZHOU Zhongfa, ZHU Cancan, WANG Yanlin, XUE Bingqing, TANG Yuntao, TIAN Zhonghui
2020, 39(2): 275-285. doi: 10.11932/karst2020y03
Abstract:
The Shuanghedong cave system lies in Shuyang county, Zunyi City, northern Guizhou Province, which is the primary source of the Furong river that is the first-order tributary of the Wujiang river. This cave system is 257.4 km long, ranked as first in Asia and fifth in the world now. Around the cave, strata trend is mainly NNE with highly variable dip angles. The exposed rocks include dolomites of the Cambrian middle-upper Loushanguan formation (∈2-3l) and the Ordovician lower Tongzi formation (O1t),of which the gray dolomite and porphyrite and muddy dolomite are dominant. Overall this area belongs to a mid-subtropical monsoon climate. The Dafeng cave is a branch of the Shuanghedong cave system. Its tunnel is complex, where there are many beautiful secondary calcium carbonate sedimentary landscapes. The purpose of this work was to explore the self-purification ability of the air environment in the Dafeng cave and its response mechanism. Temperature, humidity, CO2 and concentration at three sites, 1# (Shiguangsuidao), 2# (Yemingzhu), 3# (Shenquanyulu),in the cave and temperature, humidity, rainfall and other indicators outside the cave weare monitored continuously and automatically for 10 days from September 30th to October 9th, 2017. Combined with the amount of tourists and local rainfall during the monitoring period, a mathematical statistics was made to the measurement data above. The results show that the self-purification ability of the cave air environment mainly depends on the intensity of the air exchange in the cave, especially in the extreme weather (rainy days in summer and autumn). The temperature outside the cave makes the ventilation mode change, thus strengthening air exchange between the inside and outside of the cave. Airflow exchange improves the self-purification ability of the cave environment. Nevertheless such ability remains limited. Besides the temperature and humidity, when the CO2 concentration generated by the tourists exceeds the threshold value of self-purification capacity of the cave air environment, the cumulative effect of CO2 in the cave occurs. Otherwise, the CO2 concentration in the cave returns to the background value of the cave environment. At the same time, the self-purification ability reaction time of the cave air environment will also differ due to varied cavity volume and tunnel structure, for instance such reaction time at monitoring sites 1#, 2#, and 3# of the cave is 15, 18, and 20 hours, respectively.