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2019 Vol. 38, No. 3

Display Method:
30 years international cooperation with IGCP and perspectives of karst critical zone research
ZHANG Cheng, JIANG Zhongcheng, Chris Groves, YUAN Daoxian
2019, 38(3): 301-306. doi: 10.11932/karst20190302
Abstract:
IGCP661 "the Critical Zone in Karst Systems" (2017-2021) is a successive karst related project of IGCP299, 379, 448, 513 and 598. The implementation of IGCP661 provides a fine opportunity to bring scientists in karst community together and an international cooperation platform to conduct karst critical zone monitoring work and research. Tracing back to the six karst IGCP projects, the implementation trajectory and development of those projects are in line with the earth system science in 1990s to earth critical zone science in early 21st century. The impacts of climate change and anthropogenic activities to karst systems' sustainability are always concerned over two decades. In this paper, main scientific results and progresses achieved by working groups of six karst IGCP projects were summarized, in hope of promoting the correlation of various karst critical zones and establishing a global network of monitoring sites. Following the guideline of Earth System Science and multidisciplinary cooperation, systematic methodologies, namely, the Karst Feature Complex concept was raised and adopted in IGCP299 as a tool to avoid the confusion of isomorphism that might arise in morphological correlation on karst. The Karst Dynamic System(KDS) (in Project 379), Karst Ecosystem (in Project448) were used to better understand how karst systems function, and how the water, chemical, biological and human systems interact within them. Guideline with this synthesized conceptual framework, karst study was extended to global change research field. IGCP 379 sets up a link between karst processes and global change. Carbonate rock dissolution consumed atmospheric CO2 and/or soil CO2, thus the resulting CO2 uptake could contribute to atmospheric CO2 precipitation (sink). There will be an increase on this value with further consideration of carbon-pumping effect of aquatic plants. The greatest societal contribution to karst science within the framework of the IGCP has come by way of study and training efforts in the development and protection of karst water resources, with both ecological (IGCP 448) and human (IGCP 513) dimensions. Some extension works focusing on environmental change impacts upon karst system sustainability were continued and enhanced (IGCP/SIDA598), scientists and laboratories affiliated with IGCP/SIDA 598 made contributions to quantifying the impact of biogeochemical processes and human activities such as land use change on the carbon cycle.Correlation work of IGCP661 is planned to start along the Belt and Road karst zone. Karst Technical Committee(TC319) under International Organization for Standardization , will work closely with IGCP 661 to develop technical specifications for karst critical zone monitoring, thus supporting site international correlation and network establishment.
Spatial and temporal variations of soil water δD and δ18O values in dry season in a typical karst depression of a karst graben basin, Yunnan Province, south China
HUO Weijie, PU Junbing, LI Jianhong, ZHANG Tao, WANG Sainan
2019, 38(3): 307-317. doi: 10.11932/karst20190303
Abstract:
Stable isotope compositions (δD and δ18O) of soil water can be used to reveal some important information about soil hydrology, including rainwater infiltration, evaporation, groundwater recharge and specific flow and transport processes taking place in the soil. In this study, stable hydrogen and oxygen isotope component of soil water in different months and soil depths in Niuerpo karst depression (Dong mountain, Mengzi City, Yunnan Province) were analyzed. The study aimed to revealing the spatial and temporal variation characteristics of soil water in the area and providing a scientific basis for further research of soil water movement mechanism. The results show that the δD and δ18O values range from -128.3‰ to -27.6‰ and -17.5‰ to 2.5‰, with a mean value of -96.1‰±20.7‰ and -12.3‰±3.7‰, respectively. Fractionation of δD and δ18O value of the water possibly occurs to some extent when rainwater infiltrates into the soil and then is redistributed in the soil layers. The mean values of δD and δ18O of soil water in April (-86.3‰±23.8‰ and -10.6‰±4.3‰, respectively) are significant higher than that in February (-106.1‰±9.5‰ and -14.1‰±1.6‰, respectively), which was mainly attributed to the evaporation of the soil water. Spatially, there is a difference in the composition of hydrogen and oxygen isotopes between the soil of slope land and the depression. In February, there is a significant difference in the δD and δ18O value between the slope land and the depression (p<0.05). The soil water δD and δ18O value in the depression were lighter than those in the slope. In April, there is no significant difference in δD and δ18O value of soil water between the slope land and the depression (p>0.05). The soil water δD and δ18O values in the depression are slightly lighter than those in the slope. The soil water δD and δ18O values decrease with the increases of soil depth in vertical profile. There are significant differences between shallow soil water δ18O and deep soil water δ18O. In February, the δ18O value of shallow soil water is 2.8‰ higher than that of deep soil water; in April, the δ18O value of shallow soil water is 10.5‰ higher than that of deep soil water.
Discussion on formation mechanism and age of Beijing Wali conglomerate
LIU Yuanzhang, LIU Jiurong, LIU Kai, WANG Shufang, KANG Xiaojun, ZHOU Tao, WANG Liya
2019, 38(3): 318-324. doi: 10.11932/karst20190304
Abstract:
The Wali conglomerate is a kind of special conglomerate which was found beneath the Quaternary in Wali area of Haidian district of Beijing during the geothermal exploration process in the 1960s, with the features of shallow burial, large thickness, well-developed karst and good water-bearing capacity. The lithology of it is mainly the dolomite and is quite different from the surrounding Jurassic volcanic sedimentary rocks; and it seems to be much abrupt and abnormal in the occurrence of the conglomerate. The characteristics of the Wali conglomerate mainly include four aspects. Firstly, the composition is mainly chert strip dolomite mixing with volcanic sedimentary rocks and other components, which is more complex. Secondly, the gravel sorting is poor, mainly in the form of sub-angular. Thirdly, the cementation mode belongs to porous cementation, and the cements are calcareous, siliceous and sandy substances. For the fourth, dissolution process in the conglomerate is relatively well developed, and the distribution of karst caves has a feature of stratification. Wali conglomerate is located between the Babaoshan fault and the Huangzhuang-Gaoliying fault, which are two important faults in Beijing area. The study of its formation mechanism will be helpful to deepen the understanding of the characteristics of the two major faults. Also the study has important theoretical and practical significance for the study of basic geology, regional geological structure, seismic monitoring, groundwater and geothermal development, engineering construction and so on. Because of the special structure and lithology, there is a long dispute about the formation mechanism of Beijing Wali conglomerate. There are two main different views of tectonic origin and sedimentary origins. Based on the data derived from previous and new geothermal drillings in recent years, a geological profile was constructed, from which stratigraphic alignment and structural analysis were made. It is realized that there are several reverse faults with various sizes that occurred at different stages and intercept one another; and these faults have greatly disturbed the normal sequence of rock formations in the area. This reflects that the thrusting effect of the Babaoshan fault of this section is very strong and is multiphase. On the basis of the analyses of the geological structures, the lithologic composition and structure, the development and occurrence level of karst, as well as the formation process of Beijing depression, the formation mechanism of Wali conglomerate was analyzed. Result shows that the conglomerate belongs to the fault breccia of Babaoshan fault zone that developed among the Wumishan formation of Mesoproterozoic Jixian System. The age of formation of the conglomerate is approximately the middle and late Mesozoic era.
Study on spatial distribution characteristics and influencing factors of karst depressions in Shilin county, Yunnan Province
DING Zhiqiang, YU Xiaoya, GAO Xuan, LI Yuhui
2019, 38(3): 325-335. doi: 10.11932/karst20190305
Abstract:
It is of significance to study the distribution and the factors of karst impact on the development of karst depression in the fields of geomorphology and environmental science. This paper takes Shilin county with abundant karst depressions as the study area, which is in subtropical monsoon climate zone, the south of the karst plateau in eastern Yunnan Province. The area is sandwiched between the Shizong-Mile fault and the west branch of Xiaojiang fault, and at the transition zone between the southeastern margin of Qinghai-Tibet plateau and the Beibuwan hilly plain.Based on digital elevation model (DEM), the methods of Ripley’s K function, nuclear density, buffer analysis, and spatial superposition in ArcGIS are used to analyze the distribution characteristics of the depressions and the influence of geographical environment on them. The results show that, (1) The distribution of karst depression in study area presents an aggregate pattern on a scale of 8 km, and the area can be divided into three sub-areas, namely high-density(>6?km-2), medium-density (5~6?km-2) and low-density (<5?km-2) areas. The high-density area has a total area of 308 km2, which is concentrated in two areas, namely Weihei, Muzhujing, Yusheng, Nuoyi in the east, and Hemo station and Shilin town in the northwest, with an average depression density of 7.20?km-2. The medium-density area is in the surroundings of the high-density area, including Yinai, Douhei, Southern Haiyi, and Northern Weize, with an average density of 5.74?km-2; and the low-density area is mainly at the edge of county, with an average density of 4.16?km-2. From the aspect of morphological parameters of the depression individuals, perimeter and area of them are high-density area < medium-density area < low-density area; depth and side slope are high-density area ≈ medium-density area > low-density area. (2) The spatial distribution of the depressions is controlled by the factors such as topography, geomorphology and geology. They have different quantity and density at different locations in elevation, relief, slope, rock type and fault buffer. At the altitude of 1,850~1,950 m, the maximum number of depressions is 37.1%,while the slope of 6°~12° accounts for the most as 82.0%, the relief of 100~150 m is 31.3%, and the landform classification of karst hilly zone is 34.3%. In terms of rock type, the depression density in the Quaternary deposit area is 5.8?km-2, and in dolomite area is 5.6?km-2, which are both dominant distributions due to lithostratigraphy. There are differences among the density in the buffer zone of three fault groups, with similar trend of density variation at each fault group. Tectonic joints and fractures developed in the Devonian, Carboniferous and Permian strata and the Jiuxiang, Weize and Guishan faults in study area strongly control the development of karst depressions along their long axis directions.(3) The spatial variation of the depression density is well correlated with two comprehensive indicators of regional heterogeneous structure of potential hydrological connectivity (IC) and hypsometric integral (HI). As the IC value increases, the depression density decreases, showing a significant negative correlation (R2=0.81). While with the increase of HI value, the depression density gradually increases, showing a significant positive correlation (R2=0.90).The spatial distribution of karst depressions is affected by geographical factors, and IC and HI can comprehensively reflect the distribution characteristics of depressions in study area, however, whether this law is universal still need further study.
Geochemical tracing to the dedolomitization process of Ordovician Ma-5 in the southeast of Ordos basin
LI Jingjuan, SHI Yunhe, WEI Liubin, ZHANG Chenggong, SU Zhongtang
2019, 38(3): 336-343. doi: 10.11932/karst20190306
Abstract:
The dedolomitization of the reaction of high Ca/Mg fluid with dolomite is common in many strata.However,there is little discussion of the dedolomitization process. This study uses the tracing principle of carbon, oxygen, strontium isotopes and strontium to examine such a process of secondary calcite with different colors of Ordovician Ma-5 in the southeast of Ordos basin. Results show that red calcite has the characteristics of low Sr content,high 87 Sr/86 Sr and negatively-biased c13C;while white secondary calcite exhibits high Sr content,low87 Sr/86 Sr and obviously negative bias t18O. Combined with the petrological characteristics of secondary calcite,it is inferretd that dedolomitization may has two stages,(1) A near-surface period,during which the dedolomitization occurred due to atmosphere freshwater leaching,becoming the incomplete ashed of brown-red or red secondary calcite; (2) A medium-deep burial period,further dedolomitization with the superposition influence of temperature,pressure and seaborne fluid,becoming the white secondary calcite.
Comprehensive geophysical model for water prospecting in fault fracture zone:A case study of water supply well siting at Gantianba village
LI Fu, DENG Guoshi, YUAN Jianfei, WANG Dewei, TANG Yeqi, ZHOU Yimin
2019, 38(3): 344-352. doi: 10.11932/karst2018y10
Abstract:
There is a serious shortage of water resources in the poverty-stricken areas of Wumengshan.On one hand, the demand for water supply is large and on the other hand it is difficult to locate the water sources. In this study, the aquifer environmental factors,water-bearing property and geophysical characteristics were comprehensive analyzed. As a result, borehole ZK12 was sited incorporating with the the analysis of fault zone,and the application of the methods including ground resistivity profile, magnetotelluric sounding, transient electromagnetics , IP sounding and geophysical well logging,etc. The geophysical characteristics for determining fault conductive zone was hence conducted by using the geophysical parameters such as apparent resistivity, apparent polarizability, attenuation, half-life failure, apparent visual metal factor, deviation degree, excitation ratio and etc. from which multiple level geophysical model was established. In this paper, we innovatively put forward the "multi-method, multi-parameter and multi-level" geophysical exploration method for locating critical water bearing zones for the resource demand from key villages and towns in Wumengshan with contiguous poverty and water-shortage ,and overcome the limitations of a single geophysical exploration technique in locating the resources and accurate borehole siting. Through examining borehole logging data, it is confirmed that the multiple-method geophysical exploration approach can effectively determine the depth of strata and water-bearing faults, provide experiences for the geophysical exploration for water exploration, as well as play a demonstration role in groundwater exploration.
Measurement of a stalagmite diameter and its application for paleoclimate
GAO Binsheng, HU Chaoyong
2019, 38(3): 353-360. doi: 10.11932/karst2019y16
Abstract:
Stalagmite is a good information carrier for Quaternary terrestrial climate reconstruction, which is very important for understanding the evolution of the past climate and environment. Chinese stalagmites are characterized by relatively continuous growth, accurate dating and abundant information, which provide a rare perspective for the Asian monsoon and its long-term evolution. Based on stalagmites, a series of alternative indicators have been developed, such as δ18O, δ13C, trace elements and their isotopes, organic compounds and associated isotope composition, growth rate and etc, which have been widely used in the reconstruction of palaeoclimate environment. However, as a basic feature of stalagmite morphology, the growth diameter of stalagmite has rarely been studied, and its implications for climate change need to be investigated. In this study, we first proposed a method to determine the growth diameter of stalagmites. Then, we used this method to measure the growth diameter of stalagmites at the top 35 cm section of HS4 Stalagmite in Heshang cave, Qingjiang, Hubei Province. The results were compared with the temperature and flood frequency records in the study area to explore the response of the stalagmite diameter growth to climate change. The results show that the growth of the stalagmite diameters can be well characterized by the exponential regression method based on the identification of the lamina and the measurement of the broad band of the lamina at different depths, which can be used to determine the diameter of some stalagmites with obvious lamina. The actual growth diameter of HS4 stalagmite is smaller than the theoretical calculation value, which may be related to the cave structure. The high drop of the cave increases the momentum of karst dripping water, and the splash of water drip results in the loss of effective water volume, thus the effective volume of dripping water decreases greatly and the actual diameter of HS4 stalagmite is smaller. Compared with temperature, the influence of precipitation on stalagmite diameter is more significant. Therefore, stalagmite diameter is an alternative proxy of effective precipitation, which is expected to be applied in the study of stalagmite palaeoclimate.
Characteristics of open cave environment and its influencing factors:A case study of Liangfeng cave, Guilin
WU Xia, PAN Moucheng, CAO Jianhua, ZHU Xiaoyan, ZHANG Meiliang, YANG Hui, TANG Wei, LAN Gaoyong
2019, 38(3): 361-369. doi: 10.11932/karst2018y16
Abstract:
By continuous high-frequency monitoring of the internal and external temperature, humidity and pCO2 in the Liangfeng cave of Guilin, it is found that the temperature of the cave is seasonally changed under the influence of atmosphere temperature. However, due to "buffering effect" in the cave, the range of temperature change decreases with the cave depths from the outside to the inside, and its response time varies with season. The analysis of monitoring data indicated that the seasonal variation of temperature inside the cave is significantly lower than that outside the cave. By comparing the time series of temperature inside and outside of the cave, it is found that the temperature of the cave shows a longer lag time with the increase of atmospheric temperature and a shorter lag time with the decrease of atmospheric temperature at the seasonal timescale. This difference may be affected by the "buffering effect" of the internal structure of the cave in different seasons. The pCO2 in this cave has obvious seasonal variation characteristics of high in summer and low in winter. Moreover, seasonal changes in the external atmospheric environment and seasonal activities of the animals and plants on the caves have also caused seasonal variations in the main controlling factors of pCO2 in the caves.
Variability of cave climate environment and influencing factors of the Shandong peninsula Jiutian cave
ZHENG Zhihui, WANG Qing, ZHOU Houyun, CHENG Ke, WANG Hongyan
2019, 38(3): 370-377. doi: 10.11932/karst2018y19
Abstract:
In this paper, we chooses Jiutian cave as the research object, to analyzes the characteristics and influencing factors of cave environment changes, and to discusses the influence of tourism activities and changes of external environment on the changes of cave environment in order to provide a scientific basis for the protection of tourism caves. The cave air temperature, Relative Humidity (RH) and CO2 concentration had been continuously monitored for a period of three years (from December 2011 to December 2014). The pH and Electroconductivity (EC) of the water drop point were measured for two years. The results were as follows, (1) The air temperature of Jiutian cave is slightly higher than the local average temperature. The reason is related to the tourism activities and monitoring time. The temperature in the cave shows the characteristic of low in summer and high in winter, which is related to the change of temperature outside the cave and cave ventilation. In addition, the farther away from the entrance,the smaller the temperature inside the cave is affected by the changes of the outside air temperature. (2) The relative humidity and air temperature in the cave shows negative correlation,indicating that the main influencing factor of the relative humidity in the cave is the temperature. The seasonal variation is characterized by low in winter and high in summer. (3) The CO2 concentration value of Jiutian cave is relatively high, showing the characteristics of high in summer and autumn and low in winter, which is mainly related to the change of vegetation and microbial activity and drip rate caused by climate change. The peak of CO2 concentration is mainly due to the increase in the number of tourists. (4) The pH value and electroconductivity of each monitoring point in Jiutian cave are mainly related to climate change and are sensitive to climate change. In drought years with less precipitation, monitoring point has higher pH value and lower electroconductivity value.
Groundwater occurrence condition and hydrochemical characteristics:A case study of Anlong county map sheet in Guizhou Province
QU Qiunan, SONG Xiaoqing, TANG Yujie, YANG Zhenhua
2019, 38(3): 378-387. doi: 10.11932/karst20190307
Abstract:
The development of fissures and karst caves in soluble rock strata in karst mountainous areas leads to a complex condition for groundwater occurrence, and affects the ability of water to dissolve solid substances. To have a better understanding of the relationship between groundwater occurrence and hyrochemical field in karst area, a case study was conducted in Anlong county of Guizhou Province, based on the data derived from the 1/50,000 hydrogeological mapping of Anlong country map sheet. The area is located in the transition zone between the Yangtze land mass and Youjiang orogenic belt, with a fairly complex condition in geological structure, strata and lithology. The strata of the whole area are mainly those the middle to lower Triassic, with occasional exposures of the Quaternary clay, sub-clay and the Permian clastic sedimentary rocks, which belong to typical special karst hydrogeological and geomorphic areas. Through exploration well water test and groundwater hole pumping test, we obtained the data of aquifer flow rate, drawdown, water chemical index values, then established the relationship between groundwater occurrence and the the hydrochemical characteristics, in order to explore the influence of the resource occurrence conditions on hydrochemical characteristics of the aquifer studied. Results show that the aquifers in the study area can be divided into four types, i.e. pure carbonate rock, chert-rich fractured carbonate rock, fractured clastic rock and loose primary aquifers. Hydrochemical type of the aquifers is dominated by HCO-Ca?Mg type. Except for the negative correlation between the depth of the exploration and production wells in the chert-rich carbonate rock aquifer and the concentration of Mg2+and HCO-3 ions in water (R2=-0.77/-0.74), the correlations between other ion concentrations and hydrogeological parameters (unit water inflow, drawdown) are not significant, and the coefficient R2 is less than 0.3. The total dissolved solids (TDS) and total hardness (TH) contents of the chert-rich carbonate rock aquifers and primary aquifers are lower than that of the pure carbonate rock aquifer by more than 5 mg?L-1, respectively. Furthermore, the total salinity and total hardness both with high values are concentrated in areas of the pure carbonate rock aquifers, while the low value areas are distributed in primary aquifers.
Discussion on the method of searching for safe drinking waterin high-sulfate areas of Guizhou Province
FANG Shangwu, LI Qiang, WANG Ruofan, JIAO Heng, YI Rui
2019, 38(3): 388-393. doi: 10.11932/karst20190308
Abstract:
Zhenning area is located in the southwest of Guizhou Province, which is a national key development area in the main functional zone of Guizhou Province. It is a typical karst mountainous areas, where carbonate rocks are widely distributed. The excessive sulfate content in groundwater is one of the main environmental geological problems, which makes the problem of functional water shortage quite prominent, especially drink water for local villagers. This paper discusses how to find safe drinking water in the study area. Our analysis is based on data from hydrogeological and environmental geology survey, geophysical exploration, hydrogeological drilling, water sample collection and testing. It is found that the sulfate in groundwater in this area is mainly from the T2g aquifer formation, and the sulfate content in groundwater reaches 275.42-1,100 mg?L-1, implying the water of Ⅳ-V class. Tracing by 34S isotope in groundwater shows that the sulfate is mainly from gypsum dissolution. The implementation of a " combined exploration and pumping" well ZK3 reveals that the gypsum formation is distributed in the middle and lower part of T2g1a with a thickness of about 1-1.5 m. The stratified pumping test shows that the content of SO42- in groundwater in the test section of the T2g aquifer formation is 720 mg?L-1, evaluated as V class water. The water inflow is 256.61 m3?d-1 when the depth is reduced to 11.50 m. When the groundwater aquifer of the T2g gypsum formation is penetrated and sealed, the content of SO42- in groundwater is 124 mg?L-1, the borehole self-discharge rate is 330.05 m3?d-1, and the depth is reduced to 10.80 m. In this condition the borehole water inflow reaches 628.84 m3?d-1, and the water quality is Ⅲ class. This investigation demonstrates that safe and drinkable groundwater can be found below the gypsum layer by drilling to some depth. Such a method can also be applied to other regions with similar problems of water quality.
Hydro-chemical genesis and isotope characteristics of Yangzhuang karst water system
FENG Yawei, CHEN Hongnian, BU Hua, JIA Dewang
2019, 38(3): 394-403. doi: 10.11932/karst20190309
Abstract:
Taking Yangzhuang karst groundwater system as the research object, this paper aims at evaluating groundwater resources and guiding the resource development and utilization through hydrochemical analysis and isotope test . The results show that the karst groundwater system in Yangzhuang is dominated by modern water,which mainly interacts with limestone in the course of runoff . Human activities have a great impact on groundwater quality. The karst groundwater is polluted to a certain extent,and groundwater chemical field and hydrodynamic field have changed to different degrees . It is suggested that the relevant functional departments take effective measures to restrain the further development of groundwater pollution.
Discovery and significance of water-gas pressure pulsation effect within karst cavity
MA Xiao, JIANG Xiaozhen, CAO Xichong, PAN Zongyuan
2019, 38(3): 404-410. doi: 10.11932/karst20190310
Abstract:
Through the generalization of geological model of collapse, aphysical experimental model was designed to explore the changeof water-gas pressure within the karst cavity under the conditions of both openand closed systemswhen groundwater level declined. The experimental results show that, (1) When the karst cavity is of a closed system, negative pressure with regular fluctuations appears during the declining process of groundwater. Their periodicity and amplitude of fluctuations relate well to the initial water level. (2) Once the airtight systemsuddenly turns into openone, a sudden change of water-gas pressure within karst cavity occurs. This change value could reach 3 times of original value. (3) The periodical high-frequency vibration of water-air pressure is acting on the cavity roof during the declining process of groundwater and has the characteristics of pressure pulsation.(4) The change of water-gas pressure caused by the decrease of water level under closed condition can be described by a linear function of time variable. The slope of the function is affected by the section area of karst cavity and the outlet. The intercept of the function is closely related to initial water level. The effect of high-frequency vibration of water-air pressure on overburden needs further studies,which will contribute to the formation mechanism of karst collapseand breakthroughs in prevention research.
Analysis of situation and trend of sinkhole collapse
MENG Yan, LEI Mingtang
2019, 38(3): 411-417. doi: 10.11932/karst20190311
Abstract:
The karst area is more than 3.4 million km2 in China, accounting for about 36% of the country’s land area, in which sinkhole collapse and associated disaster frequently occur. A comprehensive and systematic analysis of current situation and research trend of sinkhole collapse at home and abroad is of great significance to accurately grasp the current hot topics, and to carry out scientific and effective work towards the disaster prevention and reduction. In this paper, we analyzed current research status and trend in the field of sinkhole collapse at home and abroad using big data tool on three aspects, namely, genesis mechanism, identification and evaluation, as well as monitoring and early warning, based on the CNKI database, WOS database and China karst collapse investigation and research project database. The results show that in the past five years, the international research hotspot areas in relation to sinkhole collapse are mainly concentrated in Italy, the United States, China and Spain, among them Italy is the most concerned. Foreign countries pay more attention to the erosion and corrosion of groundwater to the genetic mechanism of sinkhole collapse, and the main factors considered include rainstorm, pumping, surface runoff and sewer leakage. Among them the use of advanced equipment such as centrifuge to study the causes of karst collapse is more distinctive. Domestic studies on the causes of karst collapse can be summarized into 10 models, including gravity, erosion, suction corrosion, blasting, vibration, load, dissolution, root corrosion, pressure difference and etc. Meanwhile, mechanical and mathematical methods, such as soil arch theory and numerical simulation, have been used to gradually improve the quantification study. In terms of early identification and evaluation, remote sensing and aerial geophysical exploration methods, such as geological radar, drilling radar and Light Detection and Ranging (LiDAR), have been widely used at home and abroad. In respect of the sinkhole monitoring and early-warning, geological radars are frequently used to scan regularly in foreign countries, while in China, groundwater dynamic and chemical conditions are mainly monitored. There have been successful cases at home and abroad such as optical fiber sensing, aerial geophysical prospecting and other new technologies and methods. In terms of research trends, the current international research hotspot of sinkhole collapse mainly focuses on the interaction between human engineering activities and karst environment, which is reflected in forecasting, risk management and emergency response. In terms of project support, the largest proportion of project financial support for sinkhole collapse research mainly comes from the National Natural Science Foundation of China (NSFC) and Geological Survey Project (GSP). At present, the NSFC accounts for the largest proportion at 43%, and GSP account for 39%, showing an increasing trend in GSP. To sum up, we should combine with human engineering activities and ecological environmental protection of the study of the karst collapse closely, pay close attention to hotspots area, and focus on scientific and technological research work in the aspects of quantitative genetic mechanisms, rapid identification of hidden hazards, fine monitoring and early warning, and aging of risk prevention and control.
Study on the development characteristics and formation mechanism of karst collapse development in Shungeng mountain, Huainan City
LI Zhihao, XU Guangquan, YU Shitao, GAO Jialin, ZHANG Haitao
2019, 38(3): 418-426. doi: 10.11932/karst2018y09
Abstract:
The Shungeng mountain of Huainan City is located in the southern margin of North China plate. The karst landforms are well developed and the geological hazards of karst collapse occur frequently, which bring great potential disasters to people’s life and property in the region. Based on the karst field geological investigation, the statistics of karst collapse characteristics and the analysis of structural geology and hydrogeological conditions in the exposed and cover areas of carbonate rocks in the area, the karst collapse development mechanism in this area is summarized. The results show that the development of karst collapse in the exposed carbonate area is mainly influenced by the multi-phase tectonic movements and lithologic assemblage in this area; and the extension of the karst collapses are mainly in NW direction and most of them are located at the interface between soluble and non-soluble rocks, of which the formation mechanism is mainly structure destruction and underground erosion. The development of karst collapse in covered carbonate rock area is mostly caused by the increase of ground structures, which leads to the increase of static load and the collapse induced by strong drainage in the mining area. The formation mechanism is dominated by effective stress failure and vacuum inhaling corrosion.
Interlayer karst reservoir characteristics and development controlling factors of Ordovician in the Xinken area,Tarim basin
LIANG Chengpeng, DAN Yong, XU Shenglin, LI Fuxiang, PANG Chunyu, WEI Jiaqi
2019, 38(3): 427-437. doi: 10.11932/karst20190301
Abstract:
The fracture zone of the Ordovician system interlayer karst area in the Xinken area of of Tarim basin is a favorable area for oil and gas exploration in the north of Tarim basin in recent years. Analysis suggests that the reservoirs in this area are dominated by fracture-hole and karst reservoirs, and mainly in the longitudinal direction of 100 m below the top surface of the Yijianfang formation. Based on sedimentary environment, paleogeomorphology reconstruction and karst conditions, it is considered that the relatively pure limestone deposited on the platform facies is the foundation of karst. The karst exposure period of Yijianfang formation formed early small pores, while during the Lianglitage exposure period, underground water in bedding was the main factor to control the formation of interlayer karst reservoirs. In the karst process, faults controlled the groundwater runoff and drainage direction, i.e. determining the distribution of the karst fracture cave reservoirs. Based on the above results, a bedding karst model for the Xinken area was established to guide oil and gas exploration of the Ordovician system in this area.
Characteristics and geological significance of middle Caledonian palaeodrainage pattern in the northwest of Tahe oilfield
XIA Yongtao, LIU Yongli, LIU Cunge, LUO Peng, XIE Chengfei, XU Shan
2019, 38(3): 438-443. doi: 10.11932/karst20190312
Abstract:
The Tahe oilfield is located in the main part of Akekulei nose arch, which is situated on the Shaya uplift, northern Tarim basin, Xinjiang. The main target reservoirs are developed within paleokarst weathering crusts at the tops of middle and lower Ordovician successions, which underwent paleokarstification from the middle Caledonian to early Hercynian periods, and formed large-scale fractured-cavern reservoirs. Large amounts of previous studies on the paleokarstification in the Tahe oilfield mainly focused on the axial zone of Akekulei nose arch, which is the major part of production and displayed intensive early Hercynian paleokarstification below the overlapping lower Carboniferous shale. While the northwest part of Tahe oilfield was supposed to locate on the low-relief northwest slope of Akekulei nose arch, and preserve a large number of production of the middle Caledonian paleokarstification, which has not attracted the attention of many scholars and has been poorly studied. Starting from the factors controlling the hydrological conditions, the authors analyzed the distribution of overlying strata,determined the atmospheric freshwater confluence characteristics of each stage of paleokarstification, and explored the paleokarstification model in the northwest of Tahe oilfield. On one hand,by comparing the upper and lower Ordovician strata with several drilling data, it is revealed that the successions overlying on the weathering crusts are correlated. Shale interval in the upper Ordovician Sangtamu formation is found locally to overlie directly on the middle-lower Ordovician carbonate successions and the successions counterpart to the Qiaerbake and Lianglitage formations are absent. This context of successions in the slope zone of Akekulei nose arch is distinct from that in the axial zone and suggests the interference of the episode II of middle Caledonian. On the other hand, 3D seismic data and related techniques were applied to identify and characterize the drainage distribution patterns of episodes of middle Caledonian paleokarstification. Based on further research of the multi-episode sedimentary and tectonic evolutions and sequences of the middle Caledonian in the northwest of Tahe oilfield, it is pointed that there are two independent drainage systems on the top of Lianglitage and Sangtamu formations of the upper Ordovician successions. This research has contributed to the identification and discrimination of drainage systems during the episode II and III of the middle Caledonian paleokarstification. It is proposed for the first time that the episode II of the middle Caledonian movement at the end of Lianglitage formation has favorable conditions for the development of paleokarstification. The model of middle Caledonian paleokarstification is established provisionally. It does provides new and favorable evidence for further studying the characteristics and evolution model of the middle Caledonian paleokarstification in the Ordovician strata of the whole Tahe area. And this research provides an important clue to revealing the development of the Ordovician fractured-cavern reservoirs in Tahe oilfield, and to predicting the exploration of high-quality reservoirs in Tarim basin.
Characteristics of fault-karst carbonate reservoirs in the Shunbei No.1 well block, Tarim basin
WU Qiqiao, LI Jingrui, CAO Fei, LIANG Bin, ZHU Xiansheng, ZHANG Qingyu, DAN Yong
2019, 38(3): 444-449. doi: 10.11932/karst20190313
Abstract:
With the deepening of exploration practice for ultra deep carbonate reservoirs in Tarim basin, a new type of karst reservoirs has been found in the peripheral slope area of the Tahe river. The Shunbei No.1well area is the main production area of the Sinopec Shunbei oilfield, which is a typical fault-karst reservoir. The area has undergone 4 stages of development, a quasi syngenetic karst process on the top surface of Yijianfang formation, bedding strata of the Lianglitage formation and the dissolution of the fractured reservoir, buried karst in the Silurian Santamu formation and the late Permian hydrothermal karst transformation of the late Hercynian. Among them, the control of the 80-120 m emptying leakage below the top surface of Yijianfang formation is the bedding fracture controlled reservoir karst period of the Lianglitage formation. At the same time, it is considered that the necessary conditions for the development of dissolving body reservoirs in the Shunbei No.1 well area is the large-scale strike-slip pull-apart fault in the development region, where the dissection reflectors in the pull-apart section extend over large distances in plane and downward to large depths, marking the high quality and high yield reservoirs; while those in the thrust section show a plywood shape with narrow transverse extension, representing a secondary reservoir space.
Study on short-term effects of sugarcane biochar on nitrogen transformation in calcareous soils in karst farmland
LAI Qianqian, YANG Lin, QIN Xinghua, TIAN Wei, WU Yanzheng, TANG Shuirong, XIE Yu, Christoph Müller, MENG Lei
2019, 38(3): 450-457. doi: 10.11932/karst2019y03
Abstract:
The effect of biochar is related to the duration of soil retention. Biochar entering the soil has an effect on nitrogen transformation process, corresponding to agronomic and environmental effects on nitrogen. The researches on the effect of biochar on nitrogen transformation of calcareous soils in karst areas of Southwest China are scarce, especially the research on various pathways of nitrogen transformation. The 15N tracing technique combined with the Markov Chain Monte Carlo(MCMC)algorithm-based numerical optimization model were used to investigate the effect of biochars on nitrogen transformation in calcareous soils, which provide theoretical basis for nitrogen transformation in this area. In this study, three treatments was designed which included biochar-1% (C1), biochar-3% (C2) and control (CK),with biochar extracted from sugarcane for the experiment to determine the gross soil N transformation rate. The results showed that biochar could rapidly increase soil pH and organic carbon. There was no significant difference in nitrogen mineralization, immobilization and heterotrophic nitrification with the addition of biochar. but the adsorption rate of NH+4 increased with the increase of biochar. The addition of biochar also increased the NH+4 release rate, but the NH+4 release rate decreased with the increase of biochar. The autotrophic nitrification rate and dissimilation reduction rate of nitrogen can be reduced by adding masses of biochar. Therefore, the application of biochar in calcareous soil can quickly achieve NH+4 adsorption, reduce the rate of autotrophic nitrification, and reduce the accumulation of NO-3 in soil, thus reducing its loss and leaching risk.
Study on fallow strategies in rocky desertifieation area of Yunnan Province
CHEN Zhantu, YANG Qingyuan
2019, 38(3): 458-465. doi: 10.11932/karst20190314
Abstract:
In spite the situation of China’s rocky desertification has been preliminarily controlled, the area of cultivated land with rocky desertification is increasing. Yunnan and Guizhou Province are the important areas of pilot experiments on the fallow system in China, but the traditional patterns of rocky desertification control lack the step of fallow, thus the land use of these regions remain unchanged. Based on the field investigations to the pilot areas, the main characteristics of the fallow pattern in Yunnan Province are summarized in this paper presented as follows. In a region not less than 33.33 hm2, sign fallow agreements with farmers. The government and farmers confirm the fallow region and area together. It is connected with adjustment of the agricultural structure and consistent with economic and social development goals. Meanwhile, the study found some problems in Yunnan’s fallow including subjective regional selection, shortage of supporting funds in county governments, massive reduction in subsidies results in a public psychological gap, and weak construction of work forces. Based on the above problems,it is suggested that, to establish a technical system for the diagnosis and identification of fallow land, to clarify the scale and timing of fallow; ease the financial pressure in county governments by strengthening the integration of agricultural projects and funds, to increase the input of supporting funds; to establish dynamic subsidy mechanism which reflects the land market price, to optimize the mode of subsidization; to improve the organization and construction of work teams; to accelerate the construction of the fallow monitoring system and timely to carry out the performance evaluation of the fallow system.
Study on dynamic changes of land use and landscape pattern in Lijiang river basin from 1985 to 2014
LIN Zengxue
2019, 38(3): 466-471. doi: 10.11932/karst20190315
Abstract:
This paper analyzes the change trends of land use in Lijing river basin from 1985 to 2014 using three periods of remote sensing data of 1985, 2000 and 2014 and the methods of dynamic degree of land use and the method of land use transfer matrix.The dynamic changes of the landscape pattern are identified by the Fragstats4.2 landscape analysis tool. The results show that the overall change of land use in this region is not large in 1985-2014, mainly exhibiting decreases of woodland, cultivated land and grassland area, and the increase of wetland, urban and rural construction land and unused land area, of which the changes concentrated in 2000-2014. Meanwhile, the degree of fragmentation and complexity increased on a landscape scale, and the degree of aggregation and patch continuity need to be improved. Besides, at the level of type, the fragmentation of woodland landscape increased, and the area of cultivated land and grassland patches increased, and the clustering of wetland, residents and urban and rural construction land was relatively high showing a concentrating distribution.