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2018 Vol. 37, No. 1

Display Method:
Vertical zoning of groundwater runoff system in karst plateau
WANG Yu
2018, 37(1): 1-8. doi: 10.11932/karst20180101
Abstract:
The vertical zoning of groundwater runoff system in karst plateau have been discovered by large number of the exposed and observational studies of mineral resource exploitation, geological exploration, cave detection, tracer tests and so on. Based on burying condition of karst aquifer, spatial pattern of groundwater runoff, groundwater dynamics and the extent and depth of groundwater circulation, the groundwater runoff system can be divided into two types and six subclasses in karst plateau. The details are as follow (Table 1). The zoning of groundwater runoff system in karst plateau is mainly determined by the sedimentary facies and sedimentary cycle of the strata, geologic structural association, topographic relief, zoning of karst development.The characteristics of shallow-circulating runoff zone are with shallower circulation underground, circulating period within one hydrogeological year and being obviously impacted by seasonal change. The deep-circulating runoff zones are with deeper circulation under ground, circulating period long as several to several decade years or more and being less or few impacted by seasonal change. The characteristics of six sub-classes are direct-viewing and distinct,which would be described in detail in the paper.
Evaluation on utilization potential of shallow geothermal energy in major cities of Guizhou
SONG Xiaoqing
2018, 37(1): 9-16. doi: 10.11932/karst20180102
Abstract:
Guizhou, a province located in the southwest of China, possesses a total area of 1,414 km2 and ten major cities including Guiyang, Zunyi, Xingyi, Tongren, Liupanshui, Kaili, Duyun, Bijie, Anshun and Gui’an. Carbonate rocks and carbonate rocks intercalating clastic rocks widely extend cutover the province, which accounts for more than 90% of the total urban planning area and an ecologically vulnerable environment in each city. As a clean, new and renewable green energy, shallow geothermal energy has many advances, such as wide distribution, large reserve and can be very helpful to solve many ecologically environmental problems of the cities in Guizhou. To evaluate the utilization potential of the shallow geothermal energy, in this paper, the geothermal environment conditions was comprehensively studied; data derived from field thermal response tests and heat physical property measurements of rock and soil bodies sampled in the major cities of Guizhou were analysed. The research results show that for the most rock samples in the major cities of Guizhou, the thermal conductivity coefficient rangs from 2.0 to 4.0 W·(m·K)-1; the thermal diffusion coefficient varies from 0.5 to 3.0 mm2·s-1. The average value of the thermal conductivity of rock and soil is in the range of 2.5-3.5 W·(m·K)-1and the thermal diffusion coefficient is 1.0-1.5 mm2·s-1. By applying volumetric calculation method, the total heat-capacity at the depth of 100 m below surface is 35.20×1013kJ·℃-1,while summer and winter heat transfer powers are 520.2×104 kW and 342.3×104 kW, respectively. In terms of resource utilization potential, the shallow geothermal energy can provide for refrigeration in summer time over an area of 7.43×108 m2 and for heating in the winter over an area of 6.51×108 m2 .
Water quantity optimal schemes of the karst aquifer recharge with multi-source water at the Yufuhe river, Ji’nan
LI Fengli, WANG Weiping, HUANG Qiang, LI Jinchao, QU Shisong, DU Juan
2018, 37(1): 17-26. doi: 10.11932/karst2017y31
Abstract:
With steady expansion of the urban area of Ji’nan City, the supply of karst groundwater has been seriously affected. Under the current background, it is a practical way and important measure to transform surface water into groundwater for solving the contradiction between the protection of springs and the security of water supply, in which the Yufuhe river basin in the west of Ji’nan plays a key role. On the basis of three groundwater recharge projects built on the Yufuhe river, it is vital to determine the reasonable recharge volume and recharge time to ensure the limestone karst water recharge and reducing the invalid quaternary pore water recharge and the discharge of surface water. This work selected the section from Zhai’ertou to South-North Bridge upstream of the Yufuhe river as the target. Combining the hydrogeological conditions and other data of strata and lithology, this section was divided into 4 sub-reaches. Using Hydrus-2D to this work numerically simulated the vertical and lateral seepages of each sub-reach, yielding good results. Then we made further simulations on three scenarios with the maximum, medium and minimum groundwater depth, respectively. The modeling permitted to establish the optimal schemes of water quantity for recharge, which suggest that when the flow is about 280,000 m3·d-1, a continuous discharge should be for 19.5 days, 10.5 days and 12.7 days in the cases of maximum, medium and minimum groundwater depth, respectively.
Study of the spatial distribution pattern and water quality characteristics of karst water resources in a typical anticlinal trough valley:A case study of Yiju river basin
ZHANG Hongbo, YANG Sen, GAN Xin, LUO Fuheng
2018, 37(1): 27-36. doi: 10.11932/karst2017y56
Abstract:
Karst springs are the mainly water sources of domestic water supply in karst mountainous areas, where anticlinal trough valley is an important part in the areas. To study the spatial distribution pattern and water quality characteristics in Chongqing karst anticline region, through the hydrogeology survey in the Yiju river basin, and combined with different hydrogeological units within the basin,of which is mainly composed of Permian and Triassic and Cambrian Ordovician aquifer, we analyzed the water quality and studied the distribution of the karst springs in different hydrogeological units. The results show that,(1) The pH value of karst spring in this basin is between 7.27 and 8.07, with the average value of 7.84 and most of them are neutral and weak alkaline. The total salinity of the samples falls in the range of 129-310 mg·L-1. The Permian and Triassic aquifer water chemistry type spring survey all belong to HCO3-Ca type water, while the Cambrian and Ordovician aquifer part spring belongs to HCO3- SO4-Ca type water, which may be related to lithology and human activities in the area; 93.8% karst spring water is of excellent and good quality, which can be used as drinking water resources. (2) The average flow rate of these karst spring is 0.84 L·s-1 and 78% of them have a flow of less than 10 L·s-1 . The average flow of large karst springs with more than 10 L·s-1 is 76.56 L·s-1. There are differences in quantity and flow of karst springs in different lithologic stratums, which shows the extreme nonuniformity of karst spring development. (3) In the basin with different hydrogeologic units, there are five preferential localities where the karst springs often occur, namely, the karst and non-karst contact zones, fault fractured zones, steep cliff, the low lying discharge areas with low confined , deep valleys and both sides of cutting canyons.
Comprehensive control on rocky desertification in karst regions of southwestern China: achievements, problems, and countermeasures
CHEN Hongsong, YUE Yuemin, WANG Kelin
2018, 37(1): 37-42. doi: 10.11932/karst2018y02
Abstract:
Rocky desertification and poverty are intertwined in karst regions of southwestern China, which is the bottleneck for regional social and economic sustainable development. In recent two decades, through carrying out vegetation restoration, soil and water conservation, and ecological immigrant, the whole expansion trend of rocky desertification has got preliminary containment from continuous increase to net decrease, and the ecological condition has achieved favorable development in karst areas of southwestern China. However, the prevention and control situation remain serious, and economic development should be considered urgently during the process of ecological control. This paper analyzes firstly the achievements and problems of rocky desertification comprehensive control, and then discusses its prevention and control countermeasures based on the improvement of people's livelihood. Next the experience and drawbacks during the first stage of karst desertification control are sorted out systematically. It is suggested that in the future, the studies should be strengthened on rocky desertification evolution and its key driving factors, the structure and function dynamics of karst critical zones, and the interaction between vegetation and hydrological processes. At the same time, vegetation restoration should be combined with the promotion of ecological service and the improvement of people's livelihood, and the ecological derivative industry in line with ecological management should be nurtured and developed to push poverty alleviation through bettering "blood-making" function. This could realize the win-win result of ecological control and poverty alleviation, and promote the regional social and economic cooperation development as well as the construction of the ecological security barrier in karst regions of southwestern China.
Characteristics of transfer and their influencing factors of heavy metals in soil-crop system of peri-urban agricultural soils of Nanning, South China
LI Jie, ZHU Lixin, KANG Zhiqiang
2018, 37(1): 43-52. doi: 10.11932/karst2018y01
Abstract:
A total of 150 pairs of concentrations of Hg、Cd、Cr、Cu、Ni、Pb and Zn in the soils、grains of rice、vegetable and corn were determined in peri-urban agricultural soils of Nanning.The results indicated the mean soil concentrations of Hg、Cd、Cr、Cu、Ni、Pb and Zn were 0.116、0.202、56.76、22.12、14.49、25.18、56.28 μg·g-1,respectively.The mean concetrations of six heavy metals in crops were 0.001 1、0.037、0.054、1.153、0.205、0.011 and 9.37 μg·g-1,respectively.Enrichment factor showed that Cd is mainly originated from human sorce;whereas Cr and Ni were controlled by natural sources.Transfer ability of Pb is lower than other metals while transfer ability of Zn is higher than other metals. Transfer ability of As、Cd、Cr、Cu、Ni、Pb、Zn in soil-rice system was stronger than those in soil-vegetable and corn systems. Soil pH 、CaO、total organic matter、Fe2O3、K2O and MgO were major factors influencing metal transfer from soil to crops, whereas soil K2O and MgO contents presented a negative effect on heavy metal mobility in leafed vegetable cultivation systems.
Distribution characteristics of soil nutrient and pH in rhizosphere versus non-rhizosphere from dominant shrub along different slope position in a karst region
LIANG Yueming, SU Yirong, HE Xunyang, CHEN Xiangbi
2018, 37(1): 53-58. doi: 10.11932/karst2017y60
Abstract:
To test the effects of plant type and slope position on the distribution characteristics of nutrients and pH in plant rhizosphere and non-rhizosphere soil, two dominant shrubs (Syzygium championii and Pyracantha fortuneana) were selected in a karst region of Guangxi, Southwest China. Rhizosphere soil showed nutrients enrichment. An enrichment of soil organic carbon and available phosphorus was more pronounced in pyracantha fortunean rhizosphere, and an enrichment of soil organic carbon and total nitrogen was also found in syzygium championii rhizosphere. Significant difference in soil nutrients among slope positions was found in shrub rhizosphere and non-rhizosphere (p<0.05). In rhizosphere soil, soil organic carbon content had significantly positive correlation with total nitrogen content and significantly negative correlation with available phosphorus content (p<0.05). In non-rhizosphere soil, soil organic carbon content had significantly positive correlations with the content of total nitrogen and available phosphorus (p<0.05). A two-factor variance analysis showed that slope position had greater effect on physico-chemical properties than plant type. The above results suggested that the dominant plants in karst shrub are beneficial to improve the utilization of soil nutrients. In addition,slope position should be considered, when shrub species were used to improve soil quality in karst regions.
Contents and availability of trace elements in soils of natural forests in karst region
YANG Lin, YANG Cheng, ZHU Tongbin, XIE Yincai, QIN Xinghua, LUO Liuling, ZHU Zihong, MENG Lei, HE Qiuxiang
2018, 37(1): 59-66. doi: 10.11932/karst2017y01
Abstract:
Soil under undisturbed natural forests were sampled to investigate total and available contents of four trace elements (Cu, Fe, Mn and Zn) from four nature reserves including Maolan in Guizhou, Mengyuan and Green Stone Forest in Yunnan, and Exianling in Hainan, all of which were characterized by typical karst landform. The results showed total content of Cu, Fe, Mn and Zn reached to 0.03~0.08g·kg-1, 35.6~57.4 g·kg-1, 0.74~5.83 g·kg-1 and 0.13~1.03g·kg-1, respectively, which were significantly higher the average national background values .The available content of Cu, Fe, Mn and Zn in study areas were 1.09~3.51 mg·kg-1, 11.6~62.9 mg·kg-1, 48.3~173 mg·kg-1and 4.17~37.6 mg·kg-1, respectively. According to the evaluation standard for trace elements in soil, available contents of all four elements were at relatively high level. The average activation ratios of Cu, Fe, Mn and Zn in soils under the natural forest were 5.48%, 0.10%, 6.44% and 4.19%, respectively, indicating high supply level for Cu, Mn and Zn but low supply level for Fe. Total availability index of trace element (Et) in soil was ranked as Maolan (21.0) >Green Stone Forest (12.8) ≈Mengyuan (12.7) >Exianling (5.15). In addition, Et was significantly positively correlated with total N and organic carbon contents.
Carbon sink in rocky desertification restoration, Southwest China: A case of the peak-cluster depression areas
ZENG Faming, WU Zeyan, ZHANG Cheng, YANG Qiyong
2018, 37(1): 67-73. doi: 10.11932/karst20180103
Abstract:
The vulnerable environment and unreasonable human activities have resulted large scale of karst rocky desertification (KRD) in Southwest China, accompanging huge carbon stocks loss. To introduce the studies on carbon sink in the processes of KRD restoration projects in the peak cluster depression areas, Southwest China, this paper,based on literature analyzing, summarizes the progress and shortcomings on the carbon spatial distribution and its dynamic processes, as well as the evaluation and quantitative measurement of carbon sink under different patterns KRD restoration projects. In the next work, the second term of KRD restoration project should focus on water and soil conservation, rocky desertification prevention, and taking vegetation construction as a supplement. According to the available results on soil surveys, carbon sink mechanism, and local economic crops growing, it is a good chance to optimize the allocation of resources so that the government can make sure short-term benefits to local farmers. As a reward, more farmers will agree with the KRD restoration projects to create a sustainable and green industral chain.
Comparison of abundance of CO2 fixing microbes in paddy soil from karst and non-karst area
WANG Teng, JIN Zhenjiang, GUO Jiayi, ZHANG Shuangshuang, CHENG Yaping, ZHANG Qin, LI JinCheng
2018, 37(1): 74-80. doi: 10.11932/karst2017y58
Abstract:
oil samples were collected from paddy field in the Maocun karst experimental site to study the gene abundance of cbbLR1, cbbLG1 and cbbM, as the index of CO2 fixing bacteria in typical karst area, mixed area and nonkarst area with the utilization of realtime quantitative PCR technology. The results showed that the gene abundances of cbbLG1 in karst area were generally higher than that in non-karst area, and the maximum value was 1.42×109copies·g-1. The gene abundances of cbbLR1 and cbbM in mixed area were significantly higher than that in non-karst area, and the maximum values were 2.06×109 copies·g-1 and 3.35×107 copies·g-1. Correlation analysis showed that the abundance of cbbLG1 was significantly correlated with organic carbon mass fraction, total nitrogen mass fraction, and cation exchange capacity in the soil, which were significant factors that affect the gene abundance of cbbLG1. The abundance of the three cbbL genes had different sensitivity to pH, which was significantly positive correlated with the cbbLG1 gene and negatively correlated with the cbbM gene.
Experimental study on the utilization efficiency of Chlorella to Ca2+ and HCO3- in karst water
ZHANG Tao, LI Jianhong, PU Junbing, LI Rui, WU Feihong, LI Li
2018, 37(1): 81-90. doi: 10.11932/karst20180104
Abstract:
Chlorella was collected from Dalongdong cave in Shanglin county of Guangxi to study its utilization efficiency of Ca2+and HCO3- in three water bodies with different concentrations of DIC (4.6 mmol·L-1, 2.5 mmol·L-1and 0.5 mmol·L-1) in the closed system. The results show that: (1)After 7 days of cultivation in three different DIC solution of 4.6 mmol·L-1、2.5 mmol·L-1and 0.5 mmol·L-1, Chlorella biomass increased from 0.04 Abs,to 0.56 Abs,0.50 Abs and 0.44 Abs, respectively. In the environment with high HCO3-and Ca2+ concentration, Chlorella absorbed 54.95% of HCO3- in group A and 48.00% of HCO3- in group B, it also absorbed 28.26% of Ca2+ in group A and 24.14% of Ca2+in group B. In the environment with low HCO3- concentration, it was difficult for Chlorella to absorb HCO3- in group C (0.5 mmol·L-1). These findings indicate that the high concentration of HCO3- in karst reservoirs plays a role of "fertilization" on the growth of Chlorella,which is significant to the karst process-related carbon sink;(2)The amount of Ca2+ deposition caused by Chlorella photosynthesis using HCO3- was higher than the amount of Ca2+ absorbed by Chlorella photosynthesis;(3)Photosynthesis from Chlorella make δ13CDIC positive, while the respiration make δ13CDIC negative in the culture medium.
Effects of CO2 concentration gradient on carbonicanhydrase of two karst microalgae
HUANG Binghui, LI Qiang, FANG Junjia, CAO Jianhua, JIN Zhenjiang, PENG Wenjie, LU Xiaoxuan, LIANG Yueming
2018, 37(1): 91-100. doi: 10.11932/karst20180105
Abstract:
In response to the challenge of global warming, it is important to study karst microalgae and its carbonic anhydrase for greenhouse effect owing to carbon sequestration. Yaji experimental site is an independent karst hydrological-geological system located in the peak-cluster depression and the peak-forest plain border zone. The experiment was conducted on the Chlorella vulgaris and Nostoc calcicola Breb.Cultured on the spring water which sources from the limestone of Rongxian formation, the upper Devonian at the site. We compared the carbonic anhydrase activities of two different microalgae under different carbon dioxide concentrations by using the methods of Willbur and Anderson in a closed system and analyzed the changes of karst factor by using the WTW350i multifunctional water quality analyzer and the hardness and alkalinity kits. The results showed that the karst micro-algae could deal with the habitat impact of elevated carbon dioxide by rapidly regulating its carbonic anhydrase activity in the environment of less than 3% carbon dioxide concentration. The activities of carbonic anhydrase in Chlorella vulgaris was increased by 1.46 times and Nostoc calcicola Breb.was increased by 2.12 times respectively in the environment of 2.5%. The increase of carbon dioxide concentration leads to the change of karst factor, resulting in the decrease of pH, HCO3- and dissolved oxygen (DO) and the increase of electrical conductivity (EC). Karst microalgae play an important role in coping with the decrease of pH and HCO3- induced by the increase of carbon dioxide concentration. With the increase of incubation time, the pH and the HCO3- in the culture environment is recovered, indicating that the karst area is an important participant in response to global warming. With the increase of carbon dioxide concentration, karst factors have an important influence on carbonic anhydrase. The correlation between calcium ion of Nostoc calcicola Breb.and carbonic anhydrase was the highest at 48 h, but the correlation between EC and carbonic anhydrase of (Chlorella vulgaris) reached it highest at 48 h. Due to the correlation between carbonic anhydrase and calcium ion, the influence of calcium ion can not be neglected when we study the relationship between carbonic anhydrase and karst dynamics in karst area.
Research progress and prospect of karst ground collapse in China
LUO Xiaojie, SHEN Jian
2018, 37(1): 101-111. doi: 10.11932/karst20180106
Abstract:
In order to understand the theory and practice of karst ground collapse in China, this paper discusses the connotation and extension of karst ground collapses. It also reviews current research status of karst ground collapse in the aspects of mechanism, prediction, monitoring and prevention. The new research progress conducted in recent years and existing problems are summarized, from which the author proposed key ways forward for the research of karst ground collapse.
Analysis on collapse model of the karst area covered by clay in Wuhan City Jiangxia district Hongqi village
TU Jing, LI Huijuan, PENG Hui, WEI Xiong, JIA Long
2018, 37(1): 112-119. doi: 10.11932/karst20180107
Abstract:
Karst is widely distributed and karst collapses frequently happen in Wuhan City. The karst collapses used to occur along the Yangtze River in the main urban area where and the quaternary overburden over the subsidence area is of dual-layered structure with clay layer in upper and sandy one in the lower. However, in recent years, along with the development of urbanization and the intensification of human engineering activities in the exurban areas of the city, karst collapse has also occurred in the clay area, such as Jiangxia district. The karst collapse studied in this paper occurred on April 29, 2014, at 2:30 p.m. in a residential community due to a new construction project implemented at the Jiangxia district. The collapse’s area size was about 200 square meters. It caused two people missing, a drill rig buried and the building's 1# floor raft foundation completely collapsed, which put an end to the engineering construction and resulted in a large economic loss. Through a comprehensive analysis of the karst characteristics in the area, soil physical and mechanical properties, hydrogeological conditions and human engineering activities, the collapse mode is obtained. Our research findings show that the limestone surface in the subsidence area has a large number of dissolved channels and grooves which are connected by the dissolution fissure and the underlying karst cave. This led to the the red clay with poor mechanical properties in the bottom part of the ditch lost to the lower karst channel, forming a soil cave. Moreover, the foundation drilling, building load and vibration all accelerated the softening, disintegration and dissolution processes of the clay, thus accelerated the development of the soil cave. The foundation excavation reduced the thickness of clay and subsequently reduced the shear strength of the soil. Finally, collapse occurred under the action of gravity and additional load of the overlying soil. On the basis of Mohr-Coulomb criterion and plastic equilibrium theory, the force conditions of the soil were analyzed, from which the mechanical model of the collapse were gained. The results of the collapse mechanics model are verified, which are in line with the data derived from fieldwork. By comparison, firstly the calculation results show that the additional load on the ground and the reduction of clay thickness due to the foundation pit excavation are main inducing factors of the karst collapse. Secondly, the fluctuation of underground water level caused by drainage and atmospheric pressure difference play an important role in accelerating collapse occurrence. Finally, based on the collapse pattern and mechanics analysis, the prevention and control measures has been proposed ,that is ,to increase the anticollapse properties of the earth, increase the stability of the building foundations and reduce the hydrodynamics of the karst system.
Mechanism of karst collapse caused by punching pile constructionin Jiangxia Fasi karst collapse area
XIONG Zhitao, LIU Pengrui, YANG Tao, SHAO Yong
2018, 37(1): 120-129. doi: 10.11932/karst20180108
Abstract:
In September 5th, 2014, the 8-1# pile foundation construction site of Wu-Jia expressway bridge in Jiangxia Fasi collapsed and had caused large-scale ground collapse, resulting in 19 different collapse pits. Buildings were damaged and the embankment of Jinshui river also collapsed, leading to the construction rig buried and the project forced to stop for 1 year. Based on the monitoring system of Wuhan karst collapse areas, the dynamic monitoring of groundwater in multiple aquifers and monitoring of vibration points at different parts were carried out during impact hollowing in the limestone fracture zone, from which key parameters such as water level, water pressure and influence radius of fractured karst aquifer were monitored during the punching pile construction process in Jiangxia Fasi. The response of the karst aquifer water pressure to the construction process was studied, as well as the mechanisms of construction-induced overburden collapses were researched. The study shows that the Quaternary confined aquifer is deeply influenced by inner construction activities, but the variation of the water level is relatively flat. In the fractured karst acquirers which are very heterogeneous, when the karst channels are not exposed on the surface, the construction has little effect on the karst water. However, if they are exposed, the karst water level may have a sudden increase which will increase the risk of karst collapse.
Analysis of the characteristicsof self-potential anomalous in shallow karst area of Longrui valley,southern Guangxi,China
CHEN Yixiang, QIN Xiaoqun, HUANG Qibo, GAN Fuping, HAN Kai, ZHENG Zhijie, HE Dehuang, HUANG Dejian, FU Yu, JIANG Ying
2018, 37(1): 130-138. doi: 10.11932/karst2017y36
Abstract:
Under the influence of osmotic pressure, the seepage water flow filtered by depressions soil in karst valley, gradually infiltrate downward and finally discharge to karst conduits or underground river through upper karst erosion networks or karst fissures. In this process, the spontaneous polarization phenomenon or self-potential field will form by the ionic conductive materials. Therefore, the study on self-potential can be applied to explore shallow groundwater in karst valley. The study results showed that the self-potentials banded anomalies ranging from -60~-80 mv with about 40 m wide and extending from north to south with "S" shape have been observed just near the center of Longrui karst valley. On the plane view, the self-potential gradient contours present "zero" value anomalies varying from negative to positive near the top of the karst zones. The spatialdistribution of the "zero" value anomalous zones indicates the surface differences and changes of shallow karst development. Taking Line 18 as an example, the self-potentials caused by shallow karst seepage water in Longrui valley follow the potential function distribution, namely the self-potentials have reached the minimum and accordingly self-potential gradients vary from negative to positive with the shape of central symmetry which shows the "zero" value just near the top of the shallow karst zones(station 615). The self-potentials on either side of the minimum gradually weaken until go to zero due to the stations moving away from the karst zone. Shallow caves, dissolved-fissures and fault fractures were exposed at different depths by the hydrogeologic monitoring borehole. Thus it means that the self-potential can be used as an effective geophysical method for detecting shallow karst water.
Prediction model for the scale of karst cave based on back propagation artificial neural network and its application
LIU Zhenhua, FAN Hongyun, ZHU Yuze, LIU Shang
2018, 37(1): 139-145. doi: 10.11932/karst2018y03
Abstract:
In complex karst region, the size of karst cave is affected by many factors, such as geological structure, properties of soluble rock and groundwater hydrodynamic system and so on, which is characterized by high complexity and nonlinearity. Through the study of the occurrence and development of karst caves in karst area, the control factors affecting the scale of karst cave are determined and quantitatively analyzed, for which the data of proved caves are collected. In order to solve the problem with data fuzziness and descriptive formation of the karst caves, in this paper, the method of Back Propagation (BP) artificial neural network is employed to achieve the prediction of the scale of karst caves. As a BP neural network model is self-organization and self-adaptive, it is expected to handle the nonlinearity of sample data. The model is designed, tested, and applied, based on the MATLAB R2012a software. The results show that BP artificial neural network prediction model for the scale of karst cave is of high accuracy with its algorithm of good convergence.
Construction and application of geological information management system in karst hydrogeological environment
WEI Yanlan, LI Wenli, ZHOU Lixin, BI Xueli
2018, 37(1): 146-153. doi: 10.11932/karst20180109
Abstract:
In order to serve the geo-survey data management needs, in this paper,a GIS-based platform is applied to the construction of geological information management system(GIMS) for hydrogeological environment in karst area. The system aims to integrate the data derived from karst hydrogeological survey projects, including the field geological survey data, the laboratory analysis data, the spatial data and the result data; and the digitization, visualization and motion managements for the karst data/information can be realized in the form of database sharing. The GIMS include six main application modules, which are survey data management module, spatial data management module, data verification management module, drilling histogram management module, basic data management module and system data management module. The GIMS has been widely used in the hydrogeological environment and geological survey projects in karst areas organized by China Geological Survey, which will provide data support for the construction of the next karst geological cloud and global karst information platform.
Research and optimization of metal system device for conventional radioactive 14C dating
YANG Hui, LAN Gaoyong, TANG Wei, WU Xia, YING Qihe, WANG Hua
2018, 37(1): 154-158. doi: 10.11932/karst20180110
Abstract:
Radioisotope 14C dating techniques are widely used in quaternary geology, archaeology, oceanography and paleoclimate. The conventional 14C dating method can record the number of 14C atoms by βdecay low background liquid scintillation counter of a certain amount of samples in certain time inteval. As the equipment is simple and convenient, the accuracy of the test can meet the requirement of dating without being limited by the sample weight.The preparation system for 14C dating liquid scintillation method is mainly completed in the vacuum glass system, which is prone to breakage and fracture. Therefore a special welding master is needed in each laboratory to maintain and repair the vacuum glass system, which restricts the development of 14C dating techniques. This paper discusses the upgrading and transformation of the conventional 14C sample preparation system, and has developed a conventional 14C dating metal preparation system with metal material with the advantages of no glass welding, no oil pollution, easy installation and flexible disassembly. This system has solved the problems encountered in the development of conventional 14C dating ,and can help promoting the application of regular 14C dating techniques