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2016 Vol. 35, No. 1

Display Method:
The research progress and developing tendency of karst water
JIANG Guang-hui
2016, 35(1): 1-4. doi: 10.11932/karst2016y01
Abstract:
International conference on groundwater in karst was held in the Birmingham University, June 2015. Hundreds of scholars around the world took part in it and presented their newest studies. As the hosts, University of Birmingham and British Geological Survey showed their new progress on karst research in UK. It is believed that the important presentations in the conference may be representative for the development of karst hydrogeology in the future. Five topics were involved in the conference, including lithological, structural & stratigraphical influence on karst groundwater, karst groundwater system modeling, ecological system of karst groundwater, human-karst groundwater interaction, as well as technologies for karst groundwater exploration. According to the presentations, new knowledge emerged one after another. For example, a new modeling method was tried to predict the position of main flow paths in a karst massif. The distributed hybrid model was discussed widely for karst water. An invertebrate ecology of Chalk groundwater was identified by the support from BGS, which set a good example for further study in this topic. A holistic perspective of karst environment was noted. In the future, research on ecosystem in karst environment will be noticeable. The accuracy of modeling prediction will be enhanced obviously. Karst environmental problems, which were closely related to human life, will be solved gradually. The current projects arranged by Chinese Geological Survey should follow the new trend appearing in the conference and obtain more functions of predicting and optimal management to serve the society actively.
A study on the influencing factors for distribution of 137Cs and 210Pb specific radioactivity in Longhetun karst depression area in Pingguo, Guangxi
YIN Jian-jun, WANG Hua, LUO Wei-qun, TANG Wei
2016, 35(1): 5-10. doi: 10.11932/karst20160102
Abstract:
137Cs and 210Pb radiometric techniques have been widely used in soil erosion research. However, due to the special characteristics of karst area, such as dual-layered structure of surface and subsurface, slowness of soil formation, thin and discontinuous layer and the erodibility of the soil and so on, the applications of 137Cs and 210Pb radiometric techniques to the karst area are limited. In this study, the Longhetun depression profiles in Guohua karst ecological experimental site, Pingguo, Guangxi was chosen as an example. Soil samples along the selected profiles were collect and the specific radioactivities of 137Cs and 210Pb were analysed. The results showed that, (1) positive correlation of 137Cs and 210Pb was found both on the surface and at depths along soil profiles; this phenomenon was largely caused by human activity and soil migration, which also caused the migration of soil composition at depth. (2) Because of the enrichment of 137Cs and 210Pb in the adjacent bare rock, the maximum values of 137Cs and 210Pb specific radioactivity were found in rock cavities which are good spaces for water accumulation. (3) The 137Cs and 210Pb specific radioactivities were relative low at the bottoms of karst depression and karst valley, for perennial runoff causes the soil erosion to happen mainly on the slope and the soil deposition happen at the bottoms. (4) The soil has been well protected in the area after the previous farmlands were returned to forestlands; and the soil from the upstream can be preserved by forest, but the underground leakage cannot be avoided due to the particularity of karst environment.
Relationship between soil physicochemical properties and soil enzyme activities in Huixian karst wetland system based on Canonical Correspondence Analysis
ZHANG Ying, LIU Chang, SONG Ang, JIN Zhen-jiang, LI Qiang
2016, 35(1): 11-18. doi: 10.11932/karst20160103
Abstract:
Wetland as an important ecological system plays an important role in regulating water and climate change, which was affected by human activities. Therefore, wetland degradation becomes a global phenomenon and the focus of many scientists. Huixian karst wetland system has the research base for comprehensive control of karst ecology and rocky desertification, belonging to original semi-disturbed wetland where in the past 20 years fertilizers have been applied to paddy field and dry land. In order to reveal the relationship between soil physicochemical properties and soil enzyme activities in Huixian karst wetland system, soil samples from three kinds of lands (wetland, paddy field and dry land) were collected. To gain a better understanding of the impact from the human and agricultural activities on the karst wetland system, a suitable evaluation method based on descriptive analysis, correlation analysis and canonical correspondence analysis (CCA) was employed. The highest content of soil organic carbon, total nitrogen, alkali-hydrolyzable nitrogen, cation exchange capacity, exchangeable calcium and exchangeable magnesium appears in the wetland, followed by the paddy field and dry land, respectively; the lowest content of available phosphorus and potassium occurs in the wetland. Therefore, the karst wetland system has an important function in the maintenance of soil carbon sink and nutrition cycle. The content of available phosphorus and potassium in wetland was lower than those in the paddy field and dry land,which was affected by human and agricultural activities. The concentrations of urease, invertase, alkaline phosphatase and cellulose are also quite high in the wetland and show a strong spatial heterogeneity. By analyzing soil factors and soil enzymes confined to wetland and paddy field of the study area, the CCA biplot shows a trend of land degradation in this area, from which it can be seen that the wetland is influenced by human activities. Wetland was first cultivated as paddy field, later it was eventually reclaimed into dry land with the decline of soil natural fertility. Therefore, among these three types of lands, the wetland has a high carbon storage function, while the paddy field has the similar one. If the ecological succession is irreversible, the best way to maintain the ecological environment of wetland system is to protect paddy field as constructed wetland. It is also important to regulate and promote carbon sequestration in karst area.
A preliminary study on soil humus in soil aggregates of natural vegetation in karst area, Maocun, Guilin
YANG Hui, BAI Bing, XIE Yin-cai, CAO Jian-hua
2016, 35(1): 19-26. doi: 10.11932/karst20160104
Abstract:
To explore the relationship between physical protection and chemical protection on soil organic carbon is helpful to reveal the mechanism of soil carbon sequestration and fertility. It could also ascertain the contribution of different components of soil aggregates, humic substances in soil carbon sequestration and soil fertility. The content of humus in soil aggregate of natural vegetation in karst area was studied. The results showed that: (1) In general, the content of soil organic carbon decreased with the increase of soil depth, and the variation of organic carbon content is different at soil depths with variation of aggregate size. (2) The contents of humic and fulvic acids in the soil aggregates are lower than that in mass soil. This may be because the soluble components of humic and fulvic acids get lost in sieving aggregates. (3) The decrease of humus content along with the soil aggregate size in the two types of natural vegetation not obvious. However the total content of humic and fulvic acids gradually increase along with the decrease of soil aggregate size, that is, the maximum content of humus is in those soils with aggregate size of less than 0.25mm. (4) HA/FA is less than 1 in both the mass soil and the aggregate of two kinds of natural vegetation, which is mainly because of the relatively high temperature, high humidity, thick vegetation coverage, strong microbial degradation of the study area.
Differences in soil nutrient and carbon pool management index under different land management and utilization modes in karst slope region
ZHANG Ya-jie, QIAN Hui-hui, LI Fu-sheng, SU Yi-rong
2016, 35(1): 27-35. doi: 10.11932/karst20160105
Abstract:
The study area, located at Huanjiang karst eco-system station of Chinese Academy of Sciences, falls into typical karst peak cluster depression landscape unit. In order to provide scientific basis for determining reasonable method of land management and utilization and further improving land quality under different slope land use conditions in karst region, the differences in soil nutrient and carbon pool management indexes in different land management and utilization conditions were investigated in this study. Six types of land use were implemented on the karst slope, via the measures of natural afforestation, maize planting, pasture planting, vegetation burning, tree/grass mowing and mowing plus root removal. Afterwards, the soil samples in 0 to 20 cm depth were collected at 5 localities respectively in the upper, middle and lower slope of each land treatment, from which the soil nutrient content, organic carbon, active organic carbon and carbon pool management indexes were measure, respectively. The results showed that the contents of soil nutrient and organic carbon and carbon pool management indexes were significantly different at different treated lands. The contents of total nitrogen, total phosphorus, available nitrogen, available potassium, organic carbon and active organic carbon in soils decreased with the increase of human interference on soils, and the above mentioned indexes under maize planting, pasture planting and mowing plus root removal treatments were significantly lower than those of natural afforestation and burning treatments, because of much more human interference on the soils. The lowest contents of total nitrogen, total phosphorus, and available nitrogen occurred on maize planting lands, while the lowest content of available potassium on both maize planting and mowing plus root removal ones. The contents of total potassium and available phosphorus in the soils reached the highest on the land after maize planting treatment, but their lowest values occurred along with the tree/grass mowing treatment. The highest content of slowly available potassium in the soils occurred on the land with afforestation treatment, followed by that of maize and pasture planting treatments, while the lowest was on tree/grass mowing treatment. The lowest contents of soil organic carbon and active organic carbon were on those associated with maize planting treatment, decreased by 37.04% and 41.14%, respectively, comparing with the contents related to afforestation treatment. Except for the afforestation, the lands with the other treatments had a significant decrease in the carbon pool management index, of which the lowest occurred on those with maize planting and burning treatments. In addition, the contents of total nitrogen, total phosphorus, total potassium, available nitrogen and organic carbon in soils decreased along with the slope altitude. From this study, it is understood that in ecological vulnerable karst region, natural afforestation is the most beneficial to the maintenance and improvement of soil nutrient and carbon pool management index. On contrary, by the increase of human interference on soils, the soil nutrient content and the carbon pool management index can be significantly reduced.
Analysis and forecast of water ecological footprint in karst area based on GRNN model
YANG Zhen-hua, SU Wei-ci, ZHAO Wei-quan, XIE Zhu-jun, LI Yan-li
2016, 35(1): 36-42. doi: 10.11932/karst20160106
Abstract:
In order to reveal the driving factors and mechanism of urban ecological footprint, evaluating and predicting the degree of sustainable utilization of water resources in karst area, the change characteristics of water ecological footprint in Guiyang City from 2002 to 2014 were analyzed, according to the hydrogeological features in karst area and its correlation with the water ecological footprint, and the GRNN model was used to predict and evaluate the water ecological footprint time series. The results showed that the water ecological footprint of Guiyang city rose from 12.79 Mhm2 in 2002 to 15.74 Mhm2 in 2014, of which the variety of water volume ecological footprint was determined by the industrial water consumption, water quality ecological footprint change was determined by the ammonia emissions. The fluctuation of the water ecological carrying capacity was obvious, and the water demand was less than the water ecological footprint, which led to the coefficient of sustainable utilization of water resources was between 0.34 and 0.61. The water ecological footprint from 2015 to 2019 in Guiyang city is predicted by the GRNN model, which show that the trend of water ecological footprint first increase and then decrease, and the water ecological carrying capacity ranged from 4.315 Mhm2 to 8.038 Mhm2. But the gap between the water ecological footprint and the carrying capacity is huge; the water resources sustainable utilization coefficient is low. Therefore, the reduction of the water ecological footprint is the key to sustainable development of the water resources in Guiyang city, of which the water ecological carrying capacity is limited in karst area.
Correlation between climatic factors and EVI based on MODIS time-series data in Guizhou
CHEN Xu, WANG Li, ZHU Hong-chun, ZHANG Miao-miao, NIU Zheng
2016, 35(1): 43-50. doi: 10.11932/karst20160107
Abstract:
To study the response of the vegetation of rocky desertification area to drought climate, this paper was focused on serious rocky desertification of karst development which is typical in Guizhou Province as the experimental area. Guizhou is located in southwest China, with longitude ranging from 103°36’ E to 109°35’E and latitude from 24°37’N to 29°13’N. The area is located in the eastern Yunnan-Guizhou Plateau with topographic low in the east and high in the west. The selection of experimental points was based on 19 benchmark standard meteorological stations which have direct rainfall record in the province (Chinese meteorological data network http://data.cma.gov.cn/). Wherein the criteria used to adjust that if a site fall in rocky desertification area can be referred to the book of "Remote sensing typical karst rocky desertification-GIS study: A case of Guizhou Province". According to the records, the drought widely occurred in southwest China in the spring of 2010, while it started in the fall of 2009 in Guizhou Province. In order to maintain the consistency of time series experimental data, the drought period is identified as from the fall of 2009 to the spring of 2010, whereas the periods from the fall of 2008 to the spring of 2009 and the autumn of 2010 to the spring of 2011 are not the drought. Using the enhanced vegetation index (EVI) as an indicator of vegetation coverage degree with the data derived from the 2008-2011 moderate resolution imaging spectroradiometer (MODIS,a spatial resolution of 250 m) ,as well as the average temperature (T) and precipitation (P) of weather station as climate factors, this paper comparatively analyzed the correlation coefficient r and F test results of the vegetation and climate factors in both karst rocky desertification area and the non-rocky desertification one. The results showed that,(1) Whether or not the sites fall in rocky desertification or non-rocky desertification area and the EVI of drought period or non-drought period, the correlation coefficient rEVI-T between EVI and climatic factors-temperature (T) were greater than 0.5 (rF=0.235,α= 0.05), which showed significant correlation of the two; (2) In non-rocky desertification area, the correlation coefficient rEVI-P of EVI in both drought period and non-drought period with the climatic factors-precipitation(P), were 0.234 and 0.212,respectively, which showed non-significant correlation of the both, but the case is contrary in rocky desertification area; (3) In a year after the drought, the correlation of the EVI in rocky desertification and non-rocky desertification regions with precipitation(P) were both significant, with the correlation coefficients rEVI-P of 0.516 and 0.489, respectively.
Comprehensive geological prediction and risk assessment of covered karst ground collapse
LUO Xiao-jie, LUO Cheng
2016, 35(1): 51-59. doi: 10.11932/karst20160108
Abstract:
To provide the basis for the prevention and control of Covered Karst Ground Collapse (CKGC), based on the mechanism of three types of ground collapse which are respectively hourglass, soil cave and soil flow, and combined karst development degree with collapse triggering factors, a comprehensive geological prediction and risk assessment method for CKGC are proposed in this paper. According to the characteristics of soil particles in deformation and collapse, the soil body on the soluble rock can basically be divided into 3 types as sand, clay soil and soft soil. The 9 kinds of karst geological structures are divided on the basis of the combination of above three types of soils. At first, according to the spatial distribution of the karst geological structures, a comprehensive geological prediction of karst ground collapse was made in combination of the degree of karst development with the possible trigger factors. As a result, the study area was divided into 3 zones, namely, high prone zone, medium prone zone and low prone zone. Secondly, based on the potential impact of collapse disaster to the surrounding environment, the CKGC risk assessment was also completed, which resulted in the study area to be divided into 3 zones too, i.e., high risk zone, medium risk zone and low risk zone. The geological theory basis for CKGC comprehensive geological prediction and risk assessment method is sufficient; and it has a good practicability and operability.
Research on influential factors of the karst collapse in the Tailai Basin of Shandong Province
WANG Yan-ling
2016, 35(1): 60-66. doi: 10.11932/karst20160109
Abstract:
The geologic disaster of karst collapse is a complicated process controlled by multiple factors. Though the karst collapse is influenced by many factors, it is largely controlled by the degree of karstification,the characteristics of overburden layers and the dynamic conditions (mainly groundwater dynamic condition). On the basis of previous studies and the latest investigation,this paper has analyzed the 3 influential factors and reveals the impact conditions and function on karst collapses. Results show that,(1) the karst collapses mostly develop in the locality with thick-layered limestone of high purity, while geological structure has an obvious control on the karst collapse; (2) the karst collapses in the study area mainly occur in Quaternary strata with multiple structures, followed by quaternary strata with unitary structure and dualistic structures. Moreover, karst the collapse occurred in the area of quaternary strata are less than 30 meters in thickness; (3) the karst collapse most frequently happen at where the cavern water level fluctuates around the bedrock surface. There is an approximately linear positive correlation between the natural logarithm of the karst collapse number and changes in cavern water level; there is also an approximately exponential positive correlation between the karst collapse number and natural logarithm of the exploitation modulus of cavern water. This paper can provide scientific basis for the integrated control of karst collapse in the study area.
A review of the research on karst and sinkhole of red beds in China
JIA Long, WU Yuan-bin, PAN Zong-yuan, YIN Ren-chao, MENG Yan, GUAN Zhen-de
2016, 35(1): 67-73. doi: 10.11932/karst20160110
Abstract:
The karst area in China is spacious and the karst types are diverse. The karst phenomena in the red beds area of south China are special. In the region, the occurrence of karst collapse has become a problem that cannot be avoided in recent years. So it is necessary to make a systematic analysis of the present situation of the research on the red-bed karst and associated karst collapses, particularly occur in red-bed area in the country. Red-bed karst mainly occurs in South China where the red clastic rocks are cemented with soluble substances or contain carbonate gravels. The characteristics of the karst red beds can be summarized as follows: 1) karst types are complex and their dissolution mechanisms are diverse; 2) the red rock is not fully cemented, with low mechanical strength and being easy to be weathered and collapse; 3) it is closely related to the geological structure. In karst red-bed area, not only soil collapse but also the bedrock collapse may occur. According to the geological structure, the red beds collapse mode can be generalized into three categories: the overburden layer collapse, the red beds cave roof collapse, and the collapse of the whole red beds. At present, the research on the karst collapse of the red beds is relatively limited. It is necessary to study the mechanism of the soluble red beds on the karst collapse in the future. Further, control measure of the red beds corrosion on the karst collapse development and distribution and impact of the soluble red beds on the karst collapse development and evolution need to be investigated, which will provide scientific basis and technical support for risk assessment and prevention treatment of the karst collapse geological hazard in red beds areas.
Hazard of water gushing caused by Nanshan Tunnel engineering, Chongqing
WEI Xing-ping, ZHANG Hong, SU Cheng-xuan
2016, 35(1): 74-80. doi: 10.11932/karst20160111
Abstract:
In this paper, the radius and inflow of water gushing are respectively analysed, by using the methods of groundwater dynamics, Goodman experiential formula and experiential analysis formula. In addition, inflow rate of the water affected by railway tunnel constructions is also comparatively analysed. The analytical results enable us to draw the conclusions as follows: (1) the radius (642m in length) of the gushing water at Nanshan tunnel is smaller than that at light rail tunnel (727m in length). The altitude of the light rail tunnel is lower than that of Nanshan tunnel, which intercepts some of water-bearing area and decreases the quantity of water flowing into Nanshan tunnel. (2) The inflow of the gushing water estimated by Coase Peskov method is much closer to the figures from field measurements. (3)The influence of water leakage at the Tushan lake is much smaller than that at the small lake, as the inspective result gained from the water leakage of Zhongliang Mountain. Tushan lake is located within the influence range of Nanshan tunnel, which is affected by Nanshan tunnel. There is a comparatively larger lake and smaller one in the Tushan lake area. The larger lake which has been formed in a quite long period of time, resulting in a thick layer of silty sediment at the bottom of the lake; and it is lightly affected by water leakage of the tunnel. On the contrary, the smaller one of Tushan lake, with a thin layer of sediment at its bottom, is greatly affected by the water leakage of the Nanshan tunnel. The karst collapse hazard within the influence range of Nanshan tunnel deserves attentions, because water leakage of the tunnel may lead to the loss of buoyant force of the rock mass. In addition, to minimize any losses due to the hazard, it is important for the public to involve in monitoring and mobilizing.
Coupled fluid flow and dissolution model and associated parameter sensitivity analysis in a single carbonate rock fracture
WU Ya-zun, LIN Yun, WAN Jun-wei, WANG Zi-jie
2016, 35(1): 81-86. doi: 10.11932/karst201601012
Abstract:
Karst groundwater system is evolved from fracture water bearing medium of carbonate rock; the evolution process of this system is determined by the initial fracture network characters and boundary conditions. In order to reveal the influence degree of fracture medium and boundary conditions on the evolution of karst system, the fracture dissolution model which coupled fluid flow and dissolution was established, and the characteristics of single fracture propagation under different boundary conditions were simulated and analyzed. The results show that the increase of fracture aperture due to karst water dissolution process, rise of hydraulic gradient, initial fracture aperture and equilibrium calcium concentration will accelerate the karst evolution. Among these parameters the initial fracture aperture influences the process most significantly, while hydraulic gradient and equilibrium calcium concentration have the same remarkable impact. Moreover, with the increase of the parameter values, the parameter sensitivity gets much smaller.
Computational model of pond re-storage times in karst valley area of Chongqing based on DEM and SCS models
ZUO Feng-lin, WEI Chao-fu
2016, 35(1): 87-97. doi: 10.11932/karst20160113
Abstract:
Two typical karst valley areas in Zhongliang and Yunfeng town of Jiu Longpo district, Chongqing are selected as the study area which is located in the middle and east sides of Zhongliangshan Mountains. The study area, with an area of 532.3 hm2 and an elevation ranging from 300 to 700 m above mean sea level, lies between the latitudes of 106°23′49″ to 106°25′06″E and the longitudes of 29°26′20″ to 29°29′47″N. The area falls in humid subtropical monsoon climate region, with an average annual precipitation of about 1,027.3 mm and an average annual temperature of 17.3 ℃. Landform types of the area are karst valley and a typical anticline low mountain, where the soil types include yellow limestone soil, dark purple clay and ore sub soil; and land use patterns are dominated by forest land and upland. Hydrologically, as no main stream and tributary run through the area, pond facilities which impound rainwater have become main sources for irrigation in this area. In fact the use of ponding water has been of significance in small scale water supply and to solve the problem of water shortage in southwest China karst region. The number of pond rainwater re-storage is an important parameter in determining the quantity of water supply. Through the analysis of current problem of irrigation systems and the computation of the number of repeated pond water impoundment, it attempts to provide a scientific guidance for future planning of ponding water system in southwest China karst region. In order to predict the repeated impoundment number, SCS model was used to simulate rainfall runoff and crop water requirement, the latter of which was computed by CROPWAT8.0 in this study. Then a water balance analysis of the pond irrigation system was performed and consequently repeated impoundment number of the ponding system was sorted out. The results showed that, (1) Calculated runoff coefficient of the study area by the SCS model was from 0.16 to 0.27, which suggested that the runoff simulated by the model was reasonable; (2) In karst valley area, it is much better to use a catchment as an analytical unit than an administrative area to calculate water supply of the pond facilities; (3) In the low flow year, rainwater can be most efficiently used by the ponds in the karst valleys with a minimum rate of surplus water as 50.98%; (4) The study area of pond re-storage times were 2.51, 2.60, 2.12 in correspondence to the rainfall frequency of 50%, 75%, 95%, respectively.
Hydrochemistry and δ13CDIC features of cave water in Naduo cave, Guizhou and their influencing factors
SHEN Wei, WANG Jian-li, WANG Jia-lu, JIANG Xian-shu, MAO Qing-ya
2016, 35(1): 98-105. doi: 10.11932/karst20160114
Abstract:
Naduo cave is located in the east of Yunnan-Guizhou Plateau, Guanling county, Anshun City of Guizhou Province, China. This region is in humid subtropical monsoon climate, with a mild and humid climate and four distinctive seasons. During the period from April 2013 to May 2014, four dripping water sites (D3, D4, D10, D11) and one pool water site (DC) have been selected for a long term monitoring in Naduo cave. In order to understand the hydrochemistry, δ13CDICfeatures and their correlation with the cave water, samples of cave water were collected monthly to measure stable carbon isotope and some other geochemical indexes. The result showed that,(1)The cave water is oversaturated to calcite in the monitoring period, which reflects the cave is at the stage of carbonate deposition. The SIc of cave water during rainy season is lower than that in dry season while its PCO2is higher. It is caused mainly by a high concentration of dissolved CO2 in the soil. Under the circumstances of suitable temperature, the precipitation had an important influence on the deposition of speleothems;(2)The water in Naduo cave can respond perfectly to the change of external climate environment. Influenced by the increase of precipitation, the concentration of dissolved CO2 in soil and the activities of plants and microorganism, the δ13CDIC values possess extraordinary seasonal characteristics, lower in summer and higher winter; (3)There is remarkable difference amongδ13CDIC values of cave waters at 5 sampling sites synchronously. Inverse correlation betweenδ13CDIC values of cave water and its corresponding contents of Ca2+, Mg2+, HCO3-, EC and SIc, respectively, has been found in cave waters. These features imply thatδ13CDIC values of cave waters are controlled by soil leaching, bedrock dissolution and prior calcite precipitation (PCP) in different extent. Therefore, the interpretation of δ13CDIC values recorded in speleothems can be more accurate if considering the effects of the above mentioned hydrogeochemical processes.
Research of karst reservoirs characteristics and paleokarst development pattern of the Ordovician Yingshan formation north-slope of Tazhong, Tarim basin area
ZHANG Qing-yu, LIANG Bin, DAN Yong, LI Jing-rui, CAO Jian-wen
2016, 35(1): 106-113. doi: 10.11932/karst2016y02
Abstract:
The study area is situated in the northern slopes of Tazhong paleo-uplift, Tarim basin, where paleokarstic features are massively developed in the carbonate rocks of Yingshan Formation of the Ordovician, with abundant oil and gas resources and a broad prospect for the exploration and development of the natural resources. The development of karst reservoir and the patterns of solution cavities and fissures were studied, based on the data derived from rock chemical analysis, core drilling, and down-hole seismic and imagining logs. The results show that thick-layered pure limestone of the top two members of Yingshan Formation belongs to strong karst suite, where corrosion hole, karst fissure and cave are developed. Post-tectonic karstification has made the region become the main place for oil-gas accumulation. The results also show that vertical karst caves and solution fissures mainly occur in the depth ranges of 0 ~ 50 m and 80 ~180 m below the Yingshan Formation, of which the karst caves substantially constitute the oil-gas reservoir in this area. This was confirmed by the venting and leaking phenomena during the well drilling. In combination with the characteristics of paleo-geomorphology, we established the development patterns of paleokarstic cave system in the area between wells ZG18 and ZG22,in order to provide a concrete geological basis for karst reservoir prediction and well exploration.
Comparative study about the characteristics of inclusions in the paleokarst fillings in the northern outcrop and underground areas of Tarim Basin
CAO Jian-wen, XIA Ri-yuan, ZHANG Qing-yu, LIANG Bin, DAN Yong
2016, 35(1): 114-124. doi: 10.11932/karst20160115
Abstract:
The Ordovician oil/gas reservoir in Tarim Basin had experienced multiple stages of water-rock interactions, so the distribution and development of the karstic reservoir are very complex. However, the characteristics of inclusions in the paleo-karst fillings can effectively indicate the changes in environments and periods of water-rock actions of the paleokarst. Based on the test of the inclusions in paleokarst fillings sampled from both outcrop area and the underground, the physical and chemical characteristics of the inclusions are summarized. From a new perspective, this paper will carry out a comparative study of the karst development over the outcrop area and the underground, repectively.. The results show that in terms of type of the karstic filling inclusions, the study area is predominated by single liquid phase and gas-liquid phase aqueous inclusions, with only a small quantity of hydrocarbon inclusions occur at the underground in Tahe Oilfield. The physical characteristics of the inclusions reflect the particular environments of the buried paleo-karst. The inclusions can be divided into five combined types according to the interaction between salinity and uniform temperature. Based on the ancient geothermal gradient, the inclusions formed in three kinds of environment (i.e., shallowly buried, medium buried, deep buried). The Ordovician carbonate rock has experienced four periods of karstification, including weathering crust karst, shallowly buried, moderately buried (the early and late) and deeply buried karsts; and the filling of karst reservoir was mainly developed in the medium burial period.