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2020 Vol. 39, No. 6

Display Method:
Chemical characteristics and circulation process of geothermal water beneath Longchuan basin, western Yunnan
HUANG Qinhui, ZHANG Hua, KANG Xiaobo, WANG Bo, LIU Haifeng, CHAI Jinlong, HUANG Zhao, WANG Yan
2020, 39(6): 793-801. doi: 10.11932/karst20200601
Abstract:
A survey of geothermic geology has been conducted to clarify the distribution of geothermal resources beneath the Longchuan basin. Results show that geothermal sources are exposed at 11 sites in this basin, in which heat reservoirs are zonal and layered type structures. Of them, the layered type appears in the central part of the basin, and the edges of each side of the basin are of zonal type. In the northwest of the basin, the heat reservoirs are obviously controlled by faults, while in the southeast joints and cracks have profound influence on the geothermal sources. The host rocks of these thermal reservoirs include metamorphic rocks, granitic glutenite and fine sandstone of Neogene Manban formation. Hydrochemical analysis suggests that geothermal water is obviously affected by atmospheric precipitation, and its circulation depth is above 1,600 m, mostly between 1,800 and 2,400 m, mainly from the surrounding mountains, with recharge distance over 1.5 km. The Nanwanhe hot spring has the highest temperature and the deepest groundwater circulation, with the longest recharge distance up to 10 km. Overall the water temperature is relatively high and water circulation is deep in the northeast and west of the basin. The heat of the geothermal water comes from the deep thermal source. It is a mixed type of geothermal water that receives groundwater recharge from mountainous areas and surface water through faults, fissures and sand and gravel pores as upwelling channels for water diversion and storage.
Water level response characteristics and runoff threshold estimation of karst depressions in a valley region, western Hubei Province
LIAO Chunlai, LUO Mingming, ZHOU Hong
2020, 39(6): 802-809. doi: 10.11932/karst20200602
Abstract:
Liujiaba and Longwan, Huangliang town, Xingshan county, Hubei Province are two karst depressions in valley region with elevations of 886 m and 997 m, and catchment areas 20.9 km2 and 1.83 km2, respectively. After rainfalls, these karst depressions runoff and transform the surface water into groundwater through the sinkholes which connect to the open channels at the bottom of the depressions, and finally discharge to the Bailong spring. To study such a hydrogeological process, rainfall stations, hydrological monitoring stations and soil-water monitoring equipment were installed in these depressions and a hydrological monitoring station constructed in the Bailong Spring. Rainfall stations record air temperature and rainfall, hydrological stations monitor water level and water temperature in the sinkholes, and soil-water monitoring equipment record the soil moisture content and electrical conductivity. Different methods were used to analyze these observational data, so as to reveal characteristics of water level response and runoff yield and their influencing factors under the condition of concentrated recharge. The results show that, (1) the water level responses in the sinkholes and karst springs have better synchronous relationships with the rainfall, expressing "sudden rise and steep drop" in hydrographs with large rainfall intensity and "slow rise and slow fall" in hydrographs with low rainfall intensity. When very heavy rainfalls happen, karst waterlogging is easy to occur due to the sinkhole’s limited drainage ability. On July 24, 2019 after a rainfall storm (86.5 mm in 3.5 hours), the water level (1.96 m) surpassed the open channel height (1.6 m) in the Longwan karst depression; (2) The Chey-Manning formula was used to transfer the water level of the open channel into flow, then the rainfall and the flow of the open channel was fitted by a mathematical equation to estimate the runoff threshold of the Liujiaba and Longwan depressions, yielding values of 7.4 mm and 10.6 mm, respectively; (3)Through the changes of soil moisture content and electrical conductivity before and after the rainfall event, the influencing factors of runoff threshold were analyzed, indicating the rainfall intensity decreases the runoff threshold, and large antecedent soil moisture could promote slope-runoff. In addition, the yield threshold is also related to the topographic slope and soil material of karst depressions, implying the yield threshold is a multi-factor coupling parameter.
Characteristics and causes of variation of karst groundwater level in the Niangziguan spring area
TANG Chunlei, JIN Hua, LIANG Yongping, ZHAO Chunhong, SHEN Haoyong, PAN Yaoyun, JING Ze
2020, 39(6): 810-816. doi: 10.11932/karst2019y31
Abstract:
The Niangziguan spring is one of the largest karst springs in north China.Its clusters are exposed in the Niangziguan town,Pingding county,Yangquan City,Shanxi, with an average annual discharge of 9.81m3s-1and catchment area about 7435.8 km2. This spring is the most important water supply source of Yangquan City,which plays an irreplaceable support in urban life and industrial and agricultural production and construction.Under the background of climate change and the increasing intensity of human activities,it is facing some challenging problems,such as the decline of spring flow,water pollution and the continuous decline of karst groundwater level. To further address this issue,based on variation monitoring data of many years, combined with the conditions of groundwater recharge, runoff and drainage,this paper analyzes the characteristics and causes of dynamic changes of karst groundwater in this area.The results show that,(1)overall the water flow declined from 1980 to 2004,then tended to be stable and slightly recovered after 2004;(2)The spatial variation of the groundwater recharge area is larger than that of the runoff area. The variation in time is divided into two stages:1980-2004 and 2005-2014.In the first stage,the water level showed a continuous decline trend,while in the second stage it experienced a slow decline with fluctuations and small rise at local places.From January 1998 to January 2004,the karst groundwater level in Longzhuang decreased by 22.9 meters,with an average annual variation of 3.82 m.From May 2005 to May 2014, it increased by 1.5 meters with average annual change -0.17 m.
Analysis of focused topics in karst hydrogeology research based on bibliometrics
GUO Yongli, ZHANG Cheng, WU Qing, QUAN Xiqiang
2020, 39(6): 817-828. doi: 10.11932/karst2020y13
Abstract:
Dynamic characteristics of the research on karst hydrogeology at home and abroad from 2011 to 2018 were analyzed by means of bibliometrics analysis. Taking karst hydrogeology, karst groundwater, karst aquifer, karst underground river, karst subterranean stream, karst underground stream, karst spring, karst geothermal water, karst thermal groundwater and karst water landscape as the key words, 1,460 papers and 918 papers from 2011 to 2018 were collected in Web of Science (WoS) and China National Knowledge Infrastructure (CNKI), respectively. Relying on the analysis function of WoS and CNKI and CiteSpace software to analyze key words, such as countries, institutions, publications and journals, it can be seen that the Institute of Karst Geology of Chinese Academy of Geological Sciences has taken full advantage of its institutional functions and professional advantages in China, and China needs to further strengthen its geographical advantages and cooperation internationally. The clustering results of key words in WoS show that the highly concerned issues of international research in the field of karst hydrogeology include "karst hydrodynamics", "karst groundwater numerical simulation", "karst hydrogeochemistry" and "karst water pollution". The clustering data show that the main research topics in CNKI are "karst water-bearing system", "karst water resources", "karst water environment" and "karst hydrological engineering". In sum, statistics and analysis of focused research topics at home and abroad point out the future and innovation direction for karst hydrogeologists.
Effects of different land use types on soil anti-erodibility in Chongqing karst depression and karst-hill peak areas
REN Xia, YAN Ningzhen, CHENG Yongyi, HUANG Xingcheng
2020, 39(6): 829-835. doi: 10.11932/karst20200603
Abstract:
The karst area in southwest China is the largest one,which is mainly located in Yunnan Province, Guizhou Province and Sichuan Province. Beibei district of Chongqing belongs to subtropical monsoon humid climate,and is controlled by the brush fold of Huayin mountain.Its geological structure is the parallel ridge valley landform of "one hill three ridge two valley",which is composed of karst depression-hills in eastern Sichuan.The carbonate rocks are mainly Triassic Jialingjiang formation (T1j), Feixianguan formation (T1f) and the Permian Maokou formation (P2m). The developed soil is yellow and brown calcareous soil. Under the influence of geology and climate, the soil is seriously eroded by chemical dissolution, gravitational and fluvial erosion.In order to explore the changes and differences of soil anti-erodibility under different land use types,and provide scientific basis for soil erosion control and ecological reconstruction in karst area of Chongqing. The topsoils of 5 land use types,including cultivated land, abandoned land, shrub-grass slope land, forest land and orchard,were selected in depression-hill peak area of Jigong karst mountain in Chongqing.Through the combination of field survey and lab analysis,11 common closely indexes related soil anti-erodibility were screened and comprehensive evaluated using the principal component analysis method.The results show that: the soil in the study area belongs to clayey to loamy soil, and the most easily eroded particles ranged from 0.05 to 0.25 mm. The optimal indexes on behalf of soil anti-erodibility are >0.25 mm aggregate destruction rate, >0.25 mm water stable aggregate content, degree of aggregation, <0.01 mm physical clay content, structural particle index and <0.001 mm clay content. That is, the lower the aggregate destruction rate >0.25 mm, the higher the content of water stable aggregates content of >0.25 mm, the degree of aggregation, the physical clay content <0.01 mm, the structural particle index and the clay content of <0.001 mm, the stronger the anti-erodibility of karst soil. According to the synthetic index analysis, 3 principal components are extracted and the comprehensive evaluation model of soil anti-erodibility was established.The order of evaluation of soil anti-erodibility was, forest land > shrub-grass slope land >abandoned land> orchard> cultivated land. It is suggested that appropriate returning cultivated land to forest or grassland in the karst area will help to reduce water and soil loss, and reasonably human activities can improve soil anti-erodibility and capacity of water and soil conservation.
Analysis on soil erodibility of different land use types in the Qingmuguan karst valley
CHEN Ying, WEI Xingping, LEI Shan
2020, 39(6): 836-844. doi: 10.11932/karst20200604
Abstract:
The purpose of this work is to investigate the physicochemical properties, erodibility and influencing factors of soil in the karst areas of Chongqing City, so as to provide references for quantitative study of soil erosion and the formulation of soil and water conservation measures, and promote regional ecological protection and land use structure adjustment. The work area is in the Qingmuguan karst valley watershed of Chongqing City. This valley formed in the southward extension of the Wentangxia anticline in the Jinyun mountains, part of the parallel ridge-valley system in eastern Sichuan. Here a large area of Triassic carbonate rock is exposed. Under the action of long-term water current dissolution, a typical karst valley landscape of "one mountain, two ridges and one trough" developed. The geological strata are composed of carbonate rock(T1j、T2l) and clastic rock(T3xj). In this work, six land use types were selected as the objects, including cultivated land, coniferous and mixed conifer-broadleaf forest, bamboo forest, garden land, wild grassland and bare land. Surface soil (0-10 cm) and profile soil (0-60 cm) were collected to analyze material composition and organic carbon content, and the soil erodibility K was calculated by the EPIC model. Results show that, (1) The erodibility K value of topsoil in the study area is between 0.0371 and 0.0605, 0.0485 on average, with a median value 0.0475 and a variation coefficient 10.71%, and the skewness and the kurtosis are less than 1; (2) The topsoil is dominated by silt, attributed to silty clay loam. The organic matter content is between 13.98 and 52.24 g.kg-1, with an average value of 29.20 g.kg-1.The K value of topsoil erodibility is negatively correlated with sand content and carbon content(P <0.01), positively correlated with silt content(P <0.01),and negatively correlated with clay content(P<0.05)significantly; (3) The topsoil erodibility K values of different land use types in order are: bare land(0.0583)>cultivated land (0.0534)>garden land(0.0483)>wild grassland(0.0478) >bamboo forest(0.0469) >mixed conifer-broadleaf forest(0.0427),with prominent differences (P < 0.05), and the coefficients of variation range from 2.7% to 6.1%. Bare land and cultivated land that are strongly influenced by human activities are the primary sources of sedimentation in the region.Vegetation restoration can effectively improve soil erosion resistance;(4)For different land use types, the average soil erodibility K value in the soil profile of cultivated land (0.0563) is significantly higher than that of wild grassland (0.0516) and forest land (0.0481) (P<0.05). While the difference of soil erodibility K values between wild grassland and forest land is not obvious.In soil profiles,the K shows relatively small values with great variations in depth range 0-35 cm,and increases with depth in 35-60 cm below the surface.
Occurrence forms of inorganic phosphorus in soils of karst wetland under different landuses and comparison of two analysis methods
CHEN Liuhuan, QIN Yingfeng, WANG Ziying, HUANG Dezhou, ZHANG Yuan, LIANG Jianhong, ZHU Jing
2020, 39(6): 845-853. doi: 10.11932/karst20200605
Abstract:
The content and speciation of phosphorus(P)determine soil fertility and the risk of P leaching from soils. This work uses standard, measurement and testing(SMT)and seven-step sequential extraction methods(“seven-step method”)to investigate the occurrence of inorganic P(In-P)in typical karst soils(paddy land,orchard,barren land)and river sediment in the Huixian karst wetland of Guilin, to analyze the effects of different land utilization on the distribution of In-P in karst soils and compares the two methods on this issue. The results show that total P content in the karst wetland soils from high to low is river sediment,orchard,paddy land,and barren land. This value is the highest in the river sediment(416.97 mg?kg-1 ),in which highly bioavailable exchangeable P(Ex-P)and iron P(Fe-P)are dominant. In the barren land soil,organic P(Or-P)and residual P(Res-P) are the major forms;while In-P content(64.45 and 47.56 mg?kg-1 for 0-20 cm and 20-40 cm depth)is the lowest in all four soils. The autologous P(Au-P),which has low bioavailability,has the highest proportion in In-P of this soil compared to that in other soils. In comparison,the surface soil of the paddy land and orchard has relatively high In-P content(276.04 and 418.19 mg?kg-1, respectively)in which Fe-P is the dominant form. In this analysis, the seven-step method has advantages in the extraction of P with complex binding states. Specifically for the karst soils,which are characterized by high Ca content and alkalinity,the seven-step method is more effective in the extraction of Ca-P. The In-P constitutes a great share in the total P in karst soils, therefore the P pool is more active. Human disturbance greatly increases the In-P content and its bioavailability. Especially,the surface orchard soil has a great potential risk of P leaching. The barren soil has low In-P content and bioavailability,indicating its high P buffering capacity. The enrichment of P in sediment via leaching suggests the sediment is a risk source for river eutrophication. In general,the seven-step method is a more suitable approach for P speciation analysis in karst soils.
Effects of microorganisms agent addition on soil microbes in different rhizosphere soils and calcium carbonate dissolution
LI Yongshuang, FAN Zhouzhou, GUO Hui, ZHOU Jinxing, PENG Xiawei
2020, 39(6): 854-862. doi: 10.11932/karst20200606
Abstract:
In this experiment,microorganisms with high-yield carbonic anhydrase(CA)in the rhizosphere soil of Jianshui county, Yunnan Province were isolated and screened,and the dissolution effect was measured. The strain with better dissolution effect was prepared into a suspension for pot experiment,permitting to explore the effects of micro-bialmetabolic activities and dissolution effects of calcium carbonate rocks on rhizosphere soils of different tree species. The results show that a strain of Serratia can be screened from the rhizosphere soil with high-yield CA and strong dissolution effect. The treatment group applying the microbial agent significantly increases the number of soil microorganisms,enhances the metabolic activity and diversity of microorganisms,and accelerates the dissolution of calcium carbonate rocks. This study aims to provide technical means for the selection of plant species and the application of microbial agents in the ecological restoration process of karst areas in the future, and provide some theoretical support for the management of ecosystems in karst areas.
Study on soil moisture variation characteristics of different economic forest lands in karst gorge area:A case study of Huajiang demonstration area in Guizhou Province
GAO Ajuan, LIU Ziqi, LI Yuan, LI Kaiping
2020, 39(6): 863-872. doi: 10.11932/karst20200607
Abstract:
The study area is located in the Guanling-Zhenfeng Huajiang demonstration area in the southwestern Guizhou Province. The total area of the study area is 51.62 km2, with the karst area of 45.39 km2, and the altitude is 500-1,200 m. It is a typical karst plateau gorge area in Guizhou with exposed and broken surface and undulating terrain. Hylocereus undulatus Britt, Zanthoxylum bungeanum and Lonicera japonica Thunb are typical economic plants in this area. In this study, this three economic forest lands were selected as the sampling plots to conduct a long-term monitoring on soil moisture and rainfall and to reveal the dynamic characteristics of the soil moisture and the influence of different economic plants on the dynamics of soil moistures along soil profile. This research is also to provide scientific basis for vegetation restoration and sustainable development of the ecological environment in karst rocky desertification area. Three observation points are equidistantly arranged in each plot with three probes installed in an observation point. A soil moisture sensor (EM 50, Meter Corporation, USA) was used to continuously monitor the volumetric soil water content. At each observation point, the probes were installed at the depth of 10 cm, 25 cm and 40 cm to the soil surface, respectively, which monitored the soil water content 24 hours a day and the monitoring was conducted in five month time from May to September, 2018. During the monitoring process, the soil moisture content was recorded at a 10-minute interval. In the meantime, the rainfall data is monitored by a small meteorological observatory (ATMOS, Meter Corporation, USA). Based on the monitoring data, the coefficient of variation of soil water storage and soil water content were calculated.SPSS 20.0 was used for statistical analysis of the data, and Origin 8.5 was used for mapping. The result showed that the variation of soil water storage in the three economic forest lands was consistent with rainfall in both quantity and time. The soil water content reached a maximum value in August and its fluctuation slightly lagged behind the precipitation. During the observation period, the soil water contents in the 40 cm deep soil layer showed a difference in the three types of land, which were Hylocereus undulatus Britt field (478.97 mm)> Lonicera japonica Thunb field (372.64 mm)> Zanthoxylum bungeanum field (322.15 mm) , respectively, with the water contents of 35.97%, 27.36%, and 23.55%. In a conclusion, the Hylocereus undulatus Britt field has the best water holding effect, followed by Lonicera japonica Thunb field, and Zanthoxylum bungeanum field, which plays an important role in improving the water and soil conservation function of the area. Therefore, in the process of rocky desertification control in Huajiang karst plateau gorge of Guizhou Province, Hylocereus undulatus Britt will be helpful to be planted in an appropriate amount to achieve the effect of ecological restoration and promote the development of local industries.
Ecological water requirements of crops in typical karst fault-depression basins:A case study of the Mengzi area, Yunnan Province
ZENG Rui, ZHANG Tao, PU Junbing, LI Jianhong, WANG Sainan
2020, 39(6): 873-882. doi: 10.11932/karst20200608
Abstract:
The Mengzi fault-depression basin is a typical karst rocky desertification area, Yunnan Province. This area has serious soil erosion and leakage, difficult groundwater utilization, and prominent ecological water shortages, which seriously affect the integrity and health of the regional ecosystem. The purpose of this study is to help better solve the problems of severe water resources shortage and ecological environment problems, and provide reasonable suggestions for the agriculture development in this area. We estimate the reference evapotranspiration, ecological water requirements, and the artificial irrigation water requirements of different crops by using the Penman-Monteith formula, crop coefficients (FAO recommended) and the effective rainfall during the same period at three observation sites (Dawazi, Duogu and Niuerpo) of Mengzi in 2018. The results show that,(1) The reference evapotranspiration of these three places were 1,346.10 mm, 1,200.00 mm and 1,064.30 mm, respectively, much more than the effective rainfall in the same period, indicating the climatic characteristics of strong evaporation, which increased the requirements of crops for water. At the same time, the reference evapotranspiration at three observation points exhibits obvious spatial and temporal differences, which make their agricultural planting conditions different;(2) The ecological water requirements quota of rice, wheat, peanut, rapeseed, soybean, potato and grape grown are much greater than the effective rainfall during the same time in Dawazi, indicating that all the crops planted there require massive irrigation to ensure their normal growth. There is a low matching degree between the kinds of planting crops and the planting background conditions, indicating that the agricultural planting structure in the basin needs to be adjusted in the future;(3) The difference between the effective rainfall and the ecological water requirements quota for corn and marigolds planted in Duogu and Niuerpo in the same period is small or even nearly matched, indicating that the planting of corn and marigold in the mountainous areas matches the local planting conditions.While the difference between the effective rainfall and the ecological water requirement of apple, flue-cured tobacco planted in Duogu and Niuerpo in the same period is large, indicating that large amounts of apples and flue-cured tobacco planted in plateau mountainous areas require more artificial irrigation;(4) The water required by most crops in their growth and development stage in the study area mainly depends on the artificial irrigation, which does not well match with the law of effective rainfall, implying that the agricultural structure and agricultural planting patterns need to be adjusted in this region.In conclusion,this study suggests that some crops with less water consumption and higher heat requirements are suitable for planting in the basin. While some crops with better ecological protection and economic benefits are suitable for planting in the karst mountainous areas.
Characteristics of leaf ecological stoichiometry in typical plant communities in karst fault-depression basins of Yunnan Province
CHEN Kehao, DU Hongmei, LIU Chunjiang
2020, 39(6): 883-893. doi: 10.11932/karst20200609
Abstract:
Plant community composition, elemental content of plants and stoicheometric characteristics are strongly influenced by geological chemistry, climate and human activities in karst areas. This study is concerned with plants sampled in the natural forest, shrub and grassland communities in a karst fault-depression basin, Mengzi,Yunnan.The purpose is to clarify the content of 12 elements and stoichiometric ratios in leaves of this area. The results show that elemental concentrations of leaves are of an order C > Ca > N > K > Mg > P > Fe > Al > Zn > Mn > Na > Cu, with significant differences in N, K, Ca, Mg, Al, Cu, Zn and Mn concentrations for plants among three communities. P content limits growth of plants in natural forest and shrub communities, and N and P contents separately or jointly affect growth of plants in grassland communities. In grassland communities, ratios C:N, C:Ca and C:Mg of plants are significantly higher, while N:P ratio lower than those in the natural forest and shrub communities.The C:Ca ratio of plants significantly differs among the three communities,with the order of grasslands > natural forests > shrubs. In statistics, 27 pairs of elements (40.9 % of total element pairs) display significant correlations.The results suggest that plants have formed unique ecological stoichiometric traits to adapt for local environmental conditions in karst fault-depression basins of Yunnan.
Characteristics and paleoenvironmental significance of Ordovician karst inclusions in the Tazhong area ,Tarim basin
ZHANG Qingyu, LI Jingrui, LIANG Bin, DAN Yong, CAO Jianwen
2020, 39(6): 894-899. doi: 10.11932/karst2020y61
Abstract:
Carbonate rock paleokarst-type reservoirs in carbonate rock are a key field of oil and gas exploration and development, which have strong heterogeneity, remaining a difficult problem throughout the world. In this aspect, the determination of palaeokarst periods is always a technical barrier in geological modeling of the palaeokarst reservoirs. At present, the methods to distinguish the development periods of ancient karst are mainly based on the characteristics of exposed ancient karst fillings. The geological structure in the Tazhong area, Tarim basin is complex, with multiple-period superimposed reformation of palaeokarstification. This work uses the honogenization temperature method on fluid inclusions filled in calcite of ancient karst to study the periods and environment of ancient karst in Ordovician carbonate rock of the Tazhong area. Four periods of ancient karstification are revealed, i.e. Caledonian, late Hercynian, Indosinian to Yanshanian and Himalayan times.The research results are of great significances to the prediction of karst reservoirs in the future.
Genesis relation of surface and underground rivers and reservoir characteristics in paleokarst drainage systems:A case study of Ordovician karst in the Tahe oilfield
ZHANG San, JIN Qiang, CHENG Fuqi, SUN Jianfang, WEI Hehua, ZHANG Xudong
2020, 39(6): 900-910. doi: 10.11932/karst2020y37
Abstract:
The Tahe oilfield lies on a slope of Ordovician karst, where the northern Tarim basin strongly uplifted in early Hercynian time,exposed Ordovician carbonate rock suffered from karstification for 56 Ma,producing complex fracture-cave reservoirs and karst landforms with numerous stone forests and canyons, as well as several karst drainage systems( surface rivers and underground rivers). The objective of this study was to reveal the genesis relationship between these surface and underground rivers and define reservoir characteristics in this area. Based on analyses to a large number of data of drilling,clogging, seismic surveys and measurement, the karst landform at the end period of karst development was restored by the method of drilling and seismic correction. And the genesis types and reservoir characteristics of surface rivers and underground rivers were analyzed by rock-minerals analysis and three-dimensional seismic carving technology. The results show that the geomorphologic high zone (watershed) formed by strike-slip faults developed in the east and west sides of the study area, the dustpan karst depression with southward opening lies between them, and a karst basin is present in the south. The northern depression is a steep slope (gradient 2.9 °) and the southern is relatively gentle (1.5 °).There are two main karst drainage formed by many tributaries developed in the depression, one is in the west that is dominated by surface rivers in the north and turns into underground rivers in the south; the other is on the east side with alternating surface (3 sections) and underground (2 sections) rivers. There are five kinds of surface rivers with different scales and fillings formed by strong erosion and dissolution, and there are no sedimentary sandstone in most surface rivers that are completely filled by the karst lacustrine marl with breccia, but no karstification, and compacted and cemented in the later period, and has almost no reservoir space. However, the underground river caves and sinkholes were filled a large amount of sandstone and mudstone, which were protected by the cave supporting, and the compaction effect was weak, among them, the porosity of sandstone reach 20%. Research suggests that the underground rivers are actually the extension of surface rivers below the ground. Originally there were sandstone deposits in surface rivers. Later on when underground rivers developed in the downstream areas,the flood washed the original sand-mudstone into the underground rivers from sinkholes,thus forming sandstone filling in karst caves of underground rivers, resulting in the high-quality oil and gas reservoirs, while almost no sandstone reservoir is present in surface rivers of Ordovician karst in the Tahe oilfield.
Characteristics and characterization of karst paleo-geomorphology and paleo-water system on the top of the Maokou formation in the Z area in southern Sichuan basin
NIE Guoquan, LI Jingrui, DAN Yong, XU Liang
2020, 39(6): 911-917. doi: 10.11932/karst20200610
Abstract:
The limestone karst reservoir of Maokou formation in southern Sichuan is relatively developed, and it is one of the important producing strata in southern Sichuan. However, the reservoirs has strong heterogeneity and high degree of fracture-cavity filling, which makes it difficult to predict reservoirs. The recovery of karst paleo-geomorphology and paleo-water system can help us to master the development and distribution of karst reservoir, which is of great significance for the oil and gas exploration of the Maokou formation in the southern Sichuan basin. In this paper, the karst paleotopography in the Z area in southern Sichuan basin is restored by the impression-trend surface method with referring sediment thickness form the top of Maokou formation to the top of Changxing formation. According to the micro-geomorphic combination form, four kinds of three-level paleogeomorphology are divided, and the north-south paleo-water system is depicted according to the theory of karst hydrogeology. The analysis shows that the hydrodynamic circumstance is quite different in different geomorphologic locations. The both sides of the fluvial are located in the runoff area, with the strongest hydrodynamic conditions and the most developed dissolution pores and fractures, which is the next reservoir exploration direction.
Characteristics of hidden karst collapse in the Zhongliangshan area of Chongqing and an approach of geophysical surveys
ZHANG Yinsong, CAO Cong, KANG Shihai, LIU Jiafu
2020, 39(6): 918-927. doi: 10.11932/karst20200611
Abstract:
The Zhongliangshan area in Chongqing has a low mountain landform, composed of the Guanyinxia anticline. It is a high-level karst with steep topography and complex geological environments, In recent years, with increasing human engineering activities, karst ground collapses occur frequently, leading to serious geological hazard, posing threat to safety of people’s life and property in this area. This work attempts to clarify the characteristics of these karst collapses. Through sampling and analyzing soil layers in the collapsed and non-collapsed areas, it is found that collapses mainly occur in loose silty clay areas with karst well developed, and suffosion is the main factor for collapse occurrence. Forward simulation on the geological model indicates that the high-density resistivity method can only detect anomalous range of 2-3 times the electrode distance, it is difficult to detect fine fractures, but it can reflect the approximate location of karst cracks, namely, it permits to delineate the funnel-shaped geological form. Then by using the seismic imaging method to divide the loose layer of surface soil , the hidden karst collapse area can be delineated. In the field survey to a residential district of the Zhongliangshan area, the high-density resistivity method is used to preliminarily screen hidden karst, and then the seismic imaging is conducted to find the area of shallow loose soil layer. In terms of such a integrated approach, the hidden collapse karst area is delineated. Finally, 10 boreholes are drilled to verify the survey results, among which 5 boreholes reveal the characteristics of the loose soil structure, in agreement with the results of geophysical surveys. It demonstrates that the approach of geophysical surveys aforementioned is feasible in detection of hidden karst collapses.
Karst depression detection using IFSAR-DEM:A tool for subsidence hazard assessment in Panglao, Bohol
Kevin L. Garas, Madonna Feliz B. Madrigal, Ross Dominic D. Agot, Mark Carlo M. Canlas, Liza Socorro J. Manzano
2020, 39(6): 928-936. doi: 10.11932/karst20200612
Abstract:
Karst studies employ high-resolution satellite images and geospatial data to identify and delineate geomorphic features that are critical to karst development and related hazard.This paper aims to determine the efficiency of Interferometric Synthetic Aperture Radar-derived Digital Elevation Model (IFSAR-DEM) to identify,quantify and characterize karst depressions using ArcGIS 10.0.The semi-automated karst depression/sinkhole detection method used water flow simulation approach that incorporated a)watershed delineation; b) sink-and-fill to extract depression features; c) sink-depth measurements and classification; and d)validation of detected karst depressions using Hyperspectral Google Satellite Image of 2013-2014 and Digital Terrain Model. The method was pre-tested in the assessment conducted in the Municipality of Panglao,Bohol.Initial closed-depression analysis using 1991 National Mapping and Resource Information Authority 1:50,000 scale topographic map counted 15 sinkholes in Panglao. Using 5 m high resolution IFSAR-DEM, there are 820 sinkholes detected, 424 of which were delineated through detailed ground truth to validate the presence of karst depressions. Ground truth included basic morphometric analysis,such as common sinkhole size,shape and depth,to eliminate false positives. Threshold values in sink depth of >1.0 m and aperture size of >10 m were designated to distinguish true sinkholes with maximum accuracy. This GIS-based tool is deemed helpful to generate high-resolution karst subsidence susceptibility map that will guide local planners and engineers,as well as policy-makers,in land use and development planning.
Characteristics and genesis of red karst in Guizhou section of Youshui river basin
JIANG Fuwei, DONG Ying, CHEN Youzhi, YU Ning, CAO Xiaojuan
2020, 39(6): 937-944. doi: 10.11932/karst20200613
Abstract:
A special set of karst landforms is present in and around the Guizhou section of the Youshui river basin. Its color is mainly red,followed white, with shape of concave-convex. This article names this type of landforms "red karst" and examines the distribution,color characteristics,and morphological features of red karst in this area. The forming force and environment of red karst are analyzed by testing the surface water pH,and CO2 content in soils and identifying rock flakes. Furthermore, the generation conditions and processes of red karst are summarized and analyzed in the paper.
Geological conditions and evolution model of red karst landscape in the Wulingshan area, China
CAO Xiaojuan, JIANG Fuwei, CHEN Youzhi, DONG Ying, YANG Hongbin
2020, 39(6): 945-951. doi: 10.11932/karst20200614
Abstract:
The Wulingshan area hosts a kind of red karst landscape with layers of fortresses and gullies embedded in a shape of palaces, which is of great value for viewing, development utilization and scientific research. Currently, there are few surveys and research reports on this type of landscape. To fill this gap, through field investigations and data analysis, this work delineated the distribution of the landscape, and analyzed the main influencing factors of its development, such as the regional geological background, stratum lithology, geological structure and dissolution, as well as its formation process. The results show that the generation of red karst landscape experienced three stages, sedimentary diagenesis, uplift and erosion, and under-soil dissolution into the landscape.