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2017 Vol. 36, No. 4

Display Method:
Temporal and spatial distributions of CO2 in soil and their influencing factors under different LUCC: A case study of the Dalongdong underground river drainage area
LAN Funing, WANG Wenjuan, WU Huaying, JIANG Zhongcheng, QIN Xiaoqun, AN Shuqing
2017, 36(4): 427-432. doi: 10.11932/karst20170401
Abstract:
The objective of this work is to further understanding the temporal and spatial distribution characteristics of CO2 in soil and its influencing factors under different land use and cover change (LUCC). We choose four types of land usage including forest land, grassland, maize land and tobacco leaf land in the Dalongdong underground river drainage area of western Hunan as examples to observe CO2 concentration of soil under these land usage conditions for one year. The results show that the soil CO2 concentrations are of the following sequence: grassland (7,527 mg·m-3)> forest land (7,197 mg·m-3)> tobacco leaf land (4,562 mg·m-3)> maize land(4,414 mg·m-3). With increasing depth of profiles, the soil CO2 in grassland and maize land usage rises first (at 10-30 cm depth) and then is stabilized (at 30-50 cm depth), and the forest land and tobacco leaf land show a trend of increasing first (at 10-30 cm depth) and then decreasing(at 30-50 cm depth). Monthly change curves of them show that the concentration of soil CO2 increases from February to August, decreases from August to December, and decreases slightly from December to February of next year. The lowest and highest values of soil CO2 concentration occur in February and August, respectively. The correlation analysis also indicates that the effect of temperature on the soil CO2 concentration is the most significant. In addition, the difference of organic carbon under different land use and the rainfall factor coupled with the temperature can pose major influence on the change of soil CO2 concentration.
Carbonic anhydrase excreted by bacteria induces the formation of carbonate minerals
LIU Lu, LI Fuchun, LI Lei, ZHANG Chonghong, LU Jiejie
2017, 36(4): 433-440. doi: 10.11932/karst20170402
Abstract:
Study on the mechanism of carbonate mineralization in the presence of microorganisms is of great significance for the global carbon cycle, soil formation and evolution and other related issues. In order to clarify the role of extracellular carbonic anhydrase (CA) excreted by bacteria in the process of carbonate mineralization, a series of chemical experiments were carried out in the CA-calcium acetate-tryptone (without carbonate) system for 120 hours. The extracellular CA from MF-2 strains was extracted through precipitation of protein by ammonium sulfate and dissolution of protein by Tris-H2SO4 buffer solution. Synchronously, a series of control experiments without CA were performed. After the experiments, the solid and the liquid phases were separated using the centrifugation method. The mineral species, its chemical composition and morphology were characterized by X-ray diffractometer (XRD) and scanning electron microscope accompanied by energy-dispersive spectrometry (SEM/EDS). The concentration of calcium ion in the solution was determined by the inductively coupled plasma optical emission spectrometer (ICP-OES). The results show that (1) the precipitate with visible amount formed in the system with extracellular CA. With the prolongation of the reaction time, the precipitate weight increased gradually, while the Ca2+ concentration in the solution decreased. The treatment results with 30% hydrogen peroxide show that carbonate mineral was the dominant component in the precipitate. The precipitate formed in the control experiments was significantly less than that in the CA experiments, which was mainly composed of organic substances. This adequately demonstrates that the extracellular CA excreted by MF-2 strain could significantly promote precipitation of carbonate minerals. (2) No crystalline formed in the initial stage of experiments (before 48th h) with CA, and calcite was dominant mineral in the precipitate formed in the middle and late stages. This was obviously different from the incubation experiments with MF-2 strain. Only vaterite formed in the latter case. (3) The mineral morphologies formed by the action of extracellular CA were rhombohedral, spherical and hemi-spherical, in which then rhombohedral mineral dominated. This was also different from the incubation experiments with MF-2 strain (spherical and bowl-shaped in the latter case). The statistical results based on several SEM photographs show that the proportion of rhombohedral-shaped minerals decreased gradually with time, from nearly 100% at 48th h to 84% at 120th h, i.e. spherical and hemi-spherical minerals gradually increased. (4) CA accelerated hydration reaction of carbon dioxide and promoted formation of carbonate minerals. The CO2 participated in the reaction might largely come from air.
Corrosion driving effects of three epilithic mosses in the Pudding karst area, Guizhou Province
ZHANG Kaiyan, LI Tongjian, ZHANG Xianqiang, SUN Min
2017, 36(4): 441-446. doi: 10.11932/karst20170403
Abstract:
Bryophytes play an important role in forest ecosystems, which are irreplaceable to soil and water conservation and the improvement of the ecological environment. Due to the ecological environment deterioration of rocky desertification in Guizhou province, serious soil erosion problem have been caused, which seriously affect the production and living of the masses. So, it is necessary to strengthen the restoration and management of the ecological environment in the region. This work took three epilithic mosses, the H.microphyllum , B.argenteum, E.leptothollum, as research materials. Using the device of simulated soil column experiment, we collected leachate and measured the carbonic anhydrase (CA) activity, electrical conductivity, pH, the content of calcium and magnesium elements and estimated the effect to limestone specimens. The results show that there are some differences about carbonic anhydrase activity of these epilithic mosses. The E. leptothollum is highest which reaches to 272.99 U·g-1.FW, whereas the minimum is 38.31 U·g-1.FW in H.microphyllum. All leachate was detected the existence of CA activity, and the leachate of B.argenteum 6d enzyme solution has the highest activity. In all, the CA activity in the 3 kinds of plants shows a tendency to decrease slightly fisrt, then increases, and finally tends to be stable. Their pH values exhibit a rising trend while electrical conductivity has downturn. The concentrations of Ca2+ and Mg2+ gradually drop with the extension of leaching time, and then tend to dynamic equilibrium after a certain time, which shows that the lithophyte has a significant enzymatic driving effect on limestone and there is a positive correlation between the dissolution rate and CA activity. This work is of great academic significance to further understanding the dynamics of CA activity produced by the metabolism of stone bryophytes in karst areas and their erosion to limestone.
Spatial-temporal evolution, mechanism and vegetation restoration of abandoned farmland in the Maolan national nature reserve
LI Yangbing, LUO Guangjie, HUANG Juan
2017, 36(4): 447-453. doi: 10.11932/karst20170404
Abstract:
To elucidate the spatial-temporal change of abandoned land and its driving mechanism is one of the most important fields in recent research of land use/change. The Maolan karst natural reserve is well preserved as a typical karst forest ecosystem and world natural heritage. This paper aims to clarify the spatial-temporal evolution of abandoned land in this area based on the high-resolution remote sensing images and field investigations, using the Arcmap and Fragstats software. The results show that in the study area, the whole area of abandoned land mainly concentrates in the buffer zone and experimental area, namely Dongjia, Biba-lapa and Banlao-dongjiu in the northwest, south and northeast of the study area. From 2005 to 2015, the spatial distribution of the abandoned land area decreased significantly, while plaque area gradually increased. Between 2005 and 2010, the number of abandoned land and distance from settlements were positively correlated. In 2015, abandoned land was mainly distributed in settlement < 200 m, 600-800 m and > 1,000 m of the buffer area, respectively. The vegetation restoration of abandoned land was mainly distributed in the core and buffer area, but there was repeated cultivation after land abandonment in the experimental area with many rural settlements and artificial disturbs. The reason of farmland abandonment in the Maolan karst natural reserve was related firstly with the decrease of rural settlement and people. Secondly, it was related with the intensive use of cultivated land in the experimental area and buffer zone, and thirdly, with the farm household livelihood diversity and transition. These results could provide complete reference for understanding the human-natural relationship evolution and ecological restoration in the Maolan karst natural reserve area.
Landscape ecological quality of different lithological regions in karst mountains:A case study in the Luodian county of Guizhou Province
SU Qijiao, AN Yulun, MA Shibin, ZHAO Yong, AN Jiakun, AN Hongfeng
2017, 36(4): 454-462. doi: 10.11932/karst20170405
Abstract:
In order to reveal the characteristics of landscape patterns and landscape ecological quality of different lithological partitions in karst mountainous area, this paper takes Luodian county of Guizhou Province as a case through analysing the data of lithologies, landscape patterns and landscape distribution, obtained from the periods of 2000, 2005, 2010 and 2015, respectively, with the intention of understanding the influence of human activities on landscape ecological quality. In the meantime, change of the landscape ecological quality was comparatively analyzed for different lithological partitions from the perspective of landscape stability and anthropogenic interference degree, which can be used to reflect the difference of landscape ecological quality in different lithological regions. The study shows that in general the landscape stability of non-karst region is higher than that of semi-karst region, while landscape stability of typical karst region is the lowest. Moreover, artificial disturbance on the landscape in semi-karst region is higher than that of non-karst region, while the disturbance degree in typical karst region is the lowest. As a result, landscape ecological quality of non-karst region is better than that of semi-karst region, whereas this quality in typical karst region is the worst. From 2000 to 2015, the landscape ecological quality tended to declines in different lithological areas. In typical karst region, this 4-period landscape ecological qualities were 0.30, 0.18, -0.24, and -0.18, respectively, which had an obvious decline between 2000 and 2010, but rose from 2010 to 2015. In semi-karst region, these ecological qualities were 0.55, 0.17, 0.32, and -0.51, respectively; they declined during this period except for years from 2005 to 2010 when they slightly rose. In non-karst region, however, the 4period values were 0.66, 0.38, 0.27, and -0.30, respectively, had been declining in the entire period since 2000. The landscape ecological qualities of semi-karst region are more susceptible to the influence of both lithology and human activity. Therefore, for ecological environment governance, measures should be taken as the basis of the differences of lithological regions where more attentions should be paid on the landscape ecological quality of semi-karst.
Root characteristics and carbon accumulation in relation to soils
HE Hongzao, ZHOU Yunchao, ZHANG Chunlai
2017, 36(4): 463-469. doi: 10.11932/karst20170406
Abstract:
To study the relationship between the input of soil organic carbon and growth of plant root systems in different soils, four kinds of plants, including Broussonetia papyrifera, Myrsine africana, Medicago sativa and Pennisetum sinese, were shifted and cultivated in calcareous and siliceous yellow soils at the cultivation base of Guizhou University in 2011. This place is of subtropical humid monsoon climate, at an altitude of 1,100 m, with an annual average temperature (MAT) of 14.9 ℃ and the annual average precipitation (MAP) of 1,178.3 mm, respectively. The monitoring system (CI-600) was installed in October 2011. For each experimental unit, a plexiglass tube, with a length of 1 meter and diameter of 0.1 meter, was inserted at an angle of 45° down to the ground, with an insert length 65 cm. During the period from January 2014 to December 2014, the root growth characteristics were observed with a plant root scanning system. The resulting data were analyzed with software WINRHIZO TRON 2009a. The dead roots were dug out for the determination of their bulk density, annual dead volume and root carbon density. The results suggest that the root system of Broussonetia papyrifera cultivated in calcareous soil grew better in comparison than that in siliceous yellow soil. It means that the soil organic carbon concentration in the karst mountainous area is larger than that in non-karst area. However, the annual dead roots volume of Medicago sativa cultivated in calcareous soil was larger than that of vegetation species, and its root has the largest contribution to soil carbon sequestration. As an arbor tree species, the root of Broussonetia papyrifera always increased with depth no matter in what soil it was cultivated with. We consider that this should be one of the key reasons why concentrations of soil organic carbon in forest lands are usually higher than those in grass lands at deeper soils. The root system of Broussonetia papyrifera cultivated in calcareous soil developed better in comparison with that of Broussonetia papyrifera cultivated in the sandy clay loam soil. In karst areas, the contributions of plants to soil carbon accumulation follow the order of Medicago sativa> Myrsine africana > Broussonetia papyrifera > Pennisetum sinese. Therefore, it is concluded that the accumulation of soil organic carbon is closely related with growth environments and species of vegetation.
Impact of human activities on land use in Dafang county, Guizhou Province
HUANG Xiaoyun, WANG Jing’ai, YIN Weixia, LI Fuhua, ZHANG Chunqin
2017, 36(4): 470-477. doi: 10.11932/karst20170407
Abstract:
Under the background of climate change, it has important significance to study the temporal and spatial changes of land use in ecologically vulnerable areas, which also can reveal the regularity of land use change and influence of human activities. Rocky desertification disaster in the main forms of water loss and soil erosion badly threats land ecological security in karst areas of South China. Dafang county is located in the northwest of Guizhou Province, China, which is one of the most serious areas of rocky desertification, whether in total area or degree of rocky desertification. In this study, Dafang county was chosen as the research area. We study temporal and spatial variations of regional land use in order to provide reference for land use structure optimization and land management in karst areas.In this work, the land use classification of TM images in 1988, 2001 and 2009 in Guizhou Province is carried out using the method of partition-layered-individual wavebands. Based on the classification results, we analyze the temporal and spatial variations of images, including spatial changes of land use types and quantity changes and effects of different altitudes and slopes on spatial and temporal variations of land use types. We also discuss the influence of human activities on these variations. The results show that the total area of cultivated land was reduced by 33%, the area of forest land increased by 34%, grassland area decreased by 11%, and the area of construction land increased by 715%, respectively. The elevations of forest land, cultivated land, grassland, construction land sequentially decrease. The influence of altitude on cultivated land and forest land is relatively large. Except for the forest land, the effect of slope on the other three kinds of land use change is relatively little. Overall, human activities are the main factors influencing the change of land use quantity and spatial pattern in Dafang county, and the natural factors such as elevation and slope have significant effects on the expansion and reduction of cultivated land and forest land.
Temporal-spatial changes of soil erosion and their relation with precipitation since the project of returning farmland to forest in Guizhou Province
YANG Tingfeng, WU Xianchun, SHANG Hailong, HE Xiang
2017, 36(4): 478-483. doi: 10.11932/karst20170408
Abstract:
Since its initiation, the environmental effect of the project invested by the Chinese government, which is a major forestry ecological project for returning farmland to forest in Guizhou Province, has attracted much attention. This study attempts to clarify the temporal and spatial variation characteristics of soil erosion and their influence on distribution of precipitation on the ground, which can reflect the effect of this project and help further controlling of soil erosion. We analyze the spatial and temporal changes of amount of sediment transport, modulus of sediment transport, sediment concentration and their relationship with precipitation in Guizhou since 2000. The coefficient of variations is used as the index to measure the magnitude of the change and the Spearman correlation method is employed for analysis. Results show that the amount of sediment transport, modulus of sediment transport, and sediment concentration have a tendency to reduce since the project initiation, of which all the inter-annual amplitudes are small, but greater than that of precipitation change. From spatial differences, the average amount of sediment transport, modulus of sediment transport, and sediment concentration in the Yangtze River basin of Guizhou are larger than those in the Pearl River basin of Guizhou, whereas the interannual variations of these parameters are smaller than those in the Pearl River basin of Guizhou. The correlation of precipitation and amount of sediment transport is 0.897,indicating a close relationship. The regression equation model is y=x1.223,which shows that the environmental effects of the project are insufficient and further efforts in construction are required.
Structure of the phytoplankton community at the Lingshui karst spring and its implications for water environment
ZHAO Hongliang, GUO Fang, LIU Shaohua
2017, 36(4): 484-491. doi: 10.11932/karst20170409
Abstract:
The submerged plants in the Lingshui lake has gradually reduced since 2010, and largely disappeared in 2013. In order to explore the causes of degradation of karst water ecosystem at this place, phytoplankton investigation and monitorin to the water environment have been conducted at the Lingshui and Luobotan karst springs in April, July and October of 2016, respectively. The results show dominant phytoplankton of 16 species belonging to 3 phyla at Lingshui and 13 phytoplankton species belonging to 3 phyla at Luobotan. The phytoplankton similarity reached 60% for both places. The basic types of phytoplankton species did not change during the three survey times, and the abundance was characterized by an order of April, July, and October from high to low. Water quality evaluation based on biodiversity indexes and chlorophyll shows that Luobotan was better than Lingshui, indicating that the water environment might degenerate after submerged plants died. RDA and correlation analysis between phytoplankton and environment shows that total nitrogen (TN) was the decisive factor for phytoplankton community. That phytoplankton has stronger absorptive capacity to nitrogen nutrient might be one of the reasons that submerged plants died in the Lingshui lake. The concentrations of HCO3- and Ca2+in the karst water environment can indicate the growth state of phytoplankton.
Evolution and spatial variation of land use conflict intensity in Qian-Gui karst mountainous areas
ZHAO Yuluan, ZHANG Ying, LI Xiubin
2017, 36(4): 492-500. doi: 10.11932/karst20170410
Abstract:
In this paper, we both use land conflict model based on PSR (Press-State-Response) to assess the evolution of land use conflict intensity and explore the change of spatial differences of land use conflict intensity at a county level and use ESDA (Exploratory Spatial Data Analysis) method for the years from 1990 to 2010 in Qian-Gui karst mountainous areas. As the results,(1) From 1990 to 2010, the phenomenon of land use conflict had increased in Qian-Gui karst mountainous areas because LUCI(Land Use Conflict Index)rose from 0.09 to 0.30;(2) In the study region, the global spatial autocorrelation of land use conflict had a significant agglomeration characteristic which appeared an enhanced trend. In addition, the global Moran’s I of the Press Index, the Response Index and LUCI were respectively 0.3179, 0.4733 and 0.1859 in phase III. Particularly, the global Moran’s I in phase II was greater than that of phase I;(3) In terms of local spatial autocorrelation, it is noted that the hotspots and sub-hotspots tended to agglomerate into city clusters which is located in Guiyang, Central Guizhou Province and Nanning City, Guangxi Zhuang Autonomous Region and its surrounding areas. However, cold spots and sub-cold spots collectively distributed in remote Qian-Gui karst peak-cluster depression areas and their surrounding districts.From the results, it is necessary to optimize the land use structure and alleviate the land use conflict, in order to improve the level of sustainable utilization of land resources.
Comparative of resident-information extraction accuracy from multi-scale remote sensing data in karst mountainous areas
AN Xiaxia, YANG Guangbin, XU Yuanhong, CHEN Zhihu, ZHANG Kai, ZHANG Bin
2017, 36(4): 501-511. doi: 10.11932/karst20170411
Abstract:
Guizhou Province hosts a typical karst landform in China, where nearly 65% of the land is karst regions. It leads to the complexity, vulnerability and diversity of Guizhou’s ecological environment because of its unique mountainous plateau terrain and the existence of karst geological conditions. The spatial distribution of the karst mountainous areas is quite different from that of other plateaus mountainous areas, which seriously affects the survival and development of the mountainous residents. Therefore, studying the satellite images with suitable resolution in the karst areas to obtain the information of the residents is very significant. In this paper, the Qinglong county is selected as the study area. The county is under the jurisdiction of Qianxi’nan Prefecture, Guizhou Province. It is located in the middle of the Yunnan-Guizhou plateau and the west of the Miaoling mountains. The main karst forms include peak-cluster depression, sinkholes, dry gutters and karst caves in Qinglong. The author selected four different resolution images as the data source, which are Y3 image (2.1 m), sentinel-2 image(10 m), GF1 image(16 m) and Landsat8 image (30 m), respectively and extracted the residential area, township and rural regions of the study area using the object-oriented classification and human-computer interaction methods. Furthermore, the accuracy of the results that three kinds of residential information extracted from the four different resolution were compared with the geographical census data obtained from the 0.5 m resolution Pleiades image through visual interpretation and field verification. The results show that, (1) In the same resolution image, the extraction error of the urban residents is smaller than that of the rural residents. Among the different resolution images, the accuracy change of the resolution of urban residential areas is the smallest, which is 23.99%, whereas the accuracy change of the rural residential areas is the biggest, up to 35.3%; (2) The total commission errors of residential information increases rapidly from 2.1 m to 30 m resolution images, which are, in order, 2.56%, 15.58%,24.50%, 32.72%. The total omission errors in the urban residential areas are obviously smaller than that in the rural residential areas, and the most wrongly type divided into other classes in three residential areas is bare lands; (3) With the reduction of image resolution, the total omission errors of residential areas are 2.86%, 18.60%, 27.99%, 37.49%, respectively, among which non-central rural residential areas are more vulnerable to the environmental impact from their surroundings, and the total omission errors of residents increase significantly with the reduction of image resolution. The final results obtained are consistent with the conclusion that the spatial resolution of the satellite sensor is proportional to the spatial resolution of the satellite sensor.
Infiltration coefficient of precipitation in karst peak-cluster depression area:A case study of Zhaidi karst underground river basin
YI Lianxing, XIA Riyuan, WANG Zhe, LU Haiping, ZHAO Liangjie
2017, 36(4): 512-517. doi: 10.11932/karst20170412
Abstract:
The precipitation infiltration coefficient α and groundwater runoff modulus M are the most basic hydrogeological parameters.In this paper,based on the high frequency monitoring data of water level, flow, precipitation of Zhaidi karst underground river basin in a hydrological year from March 2013 to February 2014,the precipitation infiltration coefficients for dry season, normal season and rainy season have been computed by means of water balance method,which are 0.352, 0.528, 0.726,respectively, and the average infiltration coefficient is 0.635. The groundwater runoff modulus are 8.32,19.80,61.15 L·s-1·km-2, respectively for the above three seasons, and the average annual runoff modulus is about 33.36 L·s-1·km-2. The calculation method and values of precipitation infiltration coefficient and groundwater runoff modulus have certain reference significance in water resources evaluation for the same karst area.
Seasonal variation of shallow groundwater characteristics and their influence factors in karst mountains: A case study of the Houzhai River in Puding County
LONG Jian, GUO Qin, LIAO Hongkai, LI Juan, LIU Lingfei, LU Yi, YAO Bin, LONG Zhifeng
2017, 36(4): 518-525. doi: 10.11932/karst20170413
Abstract:
This study focuses on the shallow groundwater of karst mountain areas in the Houzhai river in Puding county, Guizhou Province. Seasonal variations of characteristics and influence factors of shallow groundwater were analyzed. The results show that the shallow groundwater of this area contains main anion of HCO3-,SO42- and Cl-,accounting for 53%, 15% and 3% of the total ion content, and main cation of Ca2+ and Mg2+, accounting for 19% and 6% of the total ion, respectively. The hydrochemical feature is of HCO3-Ca type water. The pH is between 7.51 and 8.23. The shallow groundwater has obvious seasonal variations in terms of hydro-chemical constituents, of which the contents of HCO3-, Na+, NO3--N, Ca2+and TP have significant seasonal differences (P<0.05), while those of K+, Mg2+, Cl-, TN, NH4+-N and SO42-also seasonally fluctuate with the significant levels less than P<0.05. The chemical properties of the shallow groundwater are affected in a combined way by agricultural activity, human disturbance and rock formation lithology, of which the most typical is agricultural activity, followed by human disturbance. These two impact factors have drastically elevated the N and P concentrations in shallow groundwater in the karst mountainous areas and as a result the water quality declined.
Division of karst water protection areas based on analysis of hydrogeologic conditions
ZHAO Xianwei, WU Li, HAN Xu
2017, 36(4): 526-532. doi: 10.11932/karst2017y21
Abstract:
This paper discussed the division of water source protection zones in karst areas with complex hydro-geological conditions. Taking the Baiquan karst water system of Xingtai City, Hebei Province as an example, we analyzed the historical evolution characters of the groundwater flow field of the karst system influenced by human activities, and forecasted the variation of this field in ten years under the conditions of over exploitation by the numerical modeling method. It is found that "the artificial watershed of the Shahe River" has formed due to water drainage from mines in the spring areas, which is moving north rapidly, indicative of the seriousness of water resource shortage in the Baiquan karst area. We suggested that under complex karst hydro-geological conditions, if the protection zone is divided using the calculation flow method, it can result in waste of the protected area and the non-protection of the recharge area with carbonate exposure. On the premise of water quality protection and sustainability of water resources, we analyzed the protective capability of overlying strata of the water source and the influence on the water source of drainage from mines in the recharge area with carbonate exposure. Such recharge area should be attributed to a secondary protection zone, which breaks the traditional pattern of "the primary protection zone enclosed by the second protection zone". The overall water level of the Baiquan karst water system has increased for nearly 30 m in two years since the adjustment of the protection area, which proves that the quality and sustainability of the water source with a relatively small protection zone is guaranteed by the new division method and that the hydrogeological condition analysis is important for the division of water source protection zones in complicated areas.
Numerical simulation of karst groundwater and dynamic prediction of spring water level in the Mingshui spring area , Ji’nan City
YU Cuicui
2017, 36(4): 533-540. doi: 10.11932/karst20170415
Abstract:
The Mingshui spring area is located at the transition zone from the mountainous region to the piedmont tilting plain in central Shandong Province. It is bounded by the Wenzu fault in the west, Yuwangshan fault in the east, metamorphic rocks and the floor of Lower Cambrian series in the south, and the Ordovician limestone roof 600 m below surface in the north, respectively, with an area about 660 km2. The overall direction of karst groundwater flow is from south to north in the spring area. The spring water mainly originates from the area with outcropped limestone and abundant karst cracks in the south. The infiltration of precipitation and surface runoff result in abundant karst-crack water. This water flows along the dip direction of strata from south to north. When reaching the most low-lying area in the northern spring area, the karst ground water is blocked by the coal measures strata, and then the water ascends through cracks to become spring groups. The main recharge of karst groundwater of the Mingshui spring area is precipitation, followed by seepage supply of the Qingyang river and Dongbalou river, as well as agricultural irrigation supply. The dominate drainages are spring water drainage, artificial mining, and coal mine drainage.To provide technical basis for the rational development and protecting karst groundwater resources,and the management of karst groundwater resources in the Mingshui spring area, this work has established a 3D numerical model of groundwater for the Mingshui spring area using the groundwater modeling software GMS. Then we conducted karst groundwater numerical simulation and water balance analysis of the spring area, calculated and evaluated the karst groundwater resources, and estimated the recoverable karst groundwater amount on the condition that perennial springs spewing. On the basis of above study, this research predicted the dynamic levels of spring water using the time series analysis method. Results show that the mean annual (2003-2014) groundwater recharge of the Mingshui spring area is 1.23×108 m3·a-1, the groundwater discharge is 1.36×108 m3·a-1, and the water balance is -1.30×108 m3·a-1. The model predicts that in the next 20 years, the lowest spring water level is 55.65 m, the highest spring water level is 68.72 m, and the average spring flow is 34.6×104 m3·d-1, respectively.
Effect of urbanization on the hydrogeochemical evolution of karst groundwater system:A case of the Laolongdong watershed, Chongqing, China
ZHANG Haiyue, YANG Pingheng, WANG Jianli, LAN Jiacheng, ZHAN Zhaojun, REN Juan, ZHANG Yu
2017, 36(4): 541-549. doi: 10.11932/karst20170416
Abstract:
The underground river is in Nanshan district of Chongqing City where the karst groundwater is well-developed. There are karst depressions, sinkholes, underground rivers and exposed springs, which has the features of sensitivity and vulnerability of typical karst groundwater systems. Due to urbanization and human activities, groundwater in this area has been seriously polluted in recent years. In this paper, an underground river conduit in the karst area is taken as an example. Through analyzing the evolution of the underground, water quality deterioration and pollution sources of the groundwater, the main controlling factors of groundwater pollution in the study area are discussed, in order to protect the groundwater and provide a scientific basis for groundwater governance in this area. From 2008 to 2012, the outlet of Laolongdong underground river was chosen as a water quality minoring locality where pH value, conductivity, water temperature, potassium, sodium, calcium, magnesium, bicarbonate, chloride, nitrate, sulfate and phosphate were measured on monthly basis. The principal component analysis (PCA) was used to analyze the variation of water quality during the rainfall event in August 2011. Results indicated that in the process of urbanization, the ion concentrations of sodium, chloride, phosphate, calcium, magnesium, bicarbonate increased because of human activities. Meanwhile, the ion concentrations of nitrate, sulfate decreased due to the urbanization effect and agricultural activities. Moreover, water-rock interaction, human activities, and soil erosion played a crucial role in the hydrochemistry compositions and variation of the groundwater. Among them, dump of domestic sewage and solid wastes and the excessive uses of pesticide/fertilizers in urban residential areas are the main sources of pollutants such as potassium, sodium, chloride, sulfate, nitrate, phosphate, iron, manganese and aluminum in underground rivers. The water quality in this region varies because of the improvement of the urbanization levels and regional environment change. From the annual variation of nitrates and sulfates, the groundwater quality has been greatly improved. The karst area is sensitive and vulnerable in ecological environment. For resources protection purpose, it is essential to develop and utilize groundwater resources reasonably and reduce negative effects of groundwater pollution caused by human activities for realizing a win-win situation between the local economic benefits and sustainable development.
Dating of low-temperature geothermal karst groundwater in the stagnant area of the Liulin spring drainage
ZANG Hongfei, ZHENG Xiuqing, ZHAO Jie, WANG Wenchuan
2017, 36(4): 550-556. doi: 10.11932/karst20170417
Abstract:
The purpose of this work is to investigate the age of low-temperature geothermal karst groundwater in the stagnant area of the Liulin spring drainage. According to regional geological and hydrogeological conditions and field sampling and analysis, taking the Henggou artesian wells in the stagnant area as an example, the isotope dating techniques, including δ2H(‰), δ18O(‰), 3H(TU) and 14C (pMC)), were employed to estimate or correct the age of karst groundwater. By analyzing the relationship between 3H and 14C and the values of δ2H and δ18O, the karst groundwater in Henggou is considered to be an ancient karst groundwater, probably older than 10,000 a. The age estimated by 14C also supported this estimation. Besides, the calculated ages are 12,908 a and 9,090 a for Henggou 1 # artesian well and Henggou 2 # artesian well, respectively. Thus, the karst groundwater nearby Henggou should be recharged during the last glacial culmination.
Impact of human activities on the groundwater environment in the Mengzi basin, Yunnan Province
LU Yuxiang, HU Wei, GUO Chuandao
2017, 36(4): 557-562. doi: 10.11932/karst20170418
Abstract:
The Mengzi basin, located in southeastern Yunnan Province, is an irregular lacustrine plain with an area of 544.2 km2. The basin elevation is from 1,281 to 1,350 m, and the cover is generally 100 to 300m thick. The bottom of the basin is carbonate strata. It is the primary area of cultivated land distribution, population concentration and economic activity in Mengzi City. In recent years, the rapid development of social economy has brought about a series of problems, such as the decline of groundwater level and pollution of groundwater.This paper is based on the 1∶50,000 hydrogeological survey project of China Geological Survey. Through field investigations, sampling, pumping tests and dynamic monitoring, the influence of human activities on the groundwater environment in the Mengzi basin is studied, which is evidenced by the characteristics of groundwater environment change in the past 30 years. Compared with the previous research, in the last 30 years 20 natural springs in Quaternary cutoff in the basin. Groundwater level overall declined 5-20 m. The salinity and hardness of groundwater increased, particularly the content of Cl- and SO42-, and groundwater types became from the original two to ten. The water quality of ground water deteriorated, and the percentage of the total number of samples with good water quality and above reduced from the original 80% to 17.4% at present. The urban expansion, economic development and population expansion of the Mengzi area lead to the increase of the demand for groundwater resources, resulting in cut of spring water and decline of groundwater level. The discharge of waste water and the increase of chemical fertilizer in industrial and mining enterprises lead to the increase of salinity and hardness of groundwater, and the diversity of groundwater types. Industrial waste water and domestic sewage are discharged in a random way, and a large amount of pesticides and fertilizers are used, which leads to pollution of the surface and ground water.It is strongly suggested to control the exploitation of groundwater strictly, strengthen the monitoring and management, and rationally develop and effectively protect the groundwater resources in study area.
Micro-distribution of epikarstic aquifer fauna and its hydrological interpretation: A case study of Velika Pasica Cave in Slovenia
LIU Wei, ZHOU Hong, KE Yibing, YUAN Aihua, ZHOU Cuiying, BRANCELJ Anton
2017, 36(4): 563-571. doi: 10.11932/karst20170419
Abstract:
Intensive and long-term monitoring on hydrological parameters has been performed at four permanent dripping sites (VP1VP4) in the Velika Pasica Cave (Slovenia) from 2006 to 2013, in combination with aquatic fauna sampling. Multivariate analytical methods, such as cluster analysis and CCA method, were applied to elucidate the hydrological conditions associated with the spatial distribution of aquatic fauna within the cave and species composition at each dripping site.(1) It was found that hydrological characteristics of these four drip are distinct from each other. (2) By using cluster analysis, 12 species are divided into 4 groups, which correspond to four drips quite well. By employing CCA, the main hydrological parameters are Max and Q, which positively correlate with the first canonical axis and the drip water temperature (temp) which is negatively correlated with the first canonical axis. (3) Seven major species show different affinities to environmental parameters: abundance of Pseudocandona albicans and Speocyclops infernus,concentrating in VP1 samples which are positively correlated with the volume of discharge (Q), while abundance of Morariopsis dumonti and Bryocamptus typhlops, dominant at VP2, are negatively correlated with high discharges (Max); Byocamptus pyrenaicus and Elaphoidella millennii, dominant at VP3,with preferred moderate hydrological conditions, while Moraria varica, dominant at VP4,is positively correlated with drip water temperature. (4) The sum of eigen value by CCA only accounts for 33.8% of total eigen value, which could explain partial of the fauna distribution, but the parts of which cannot be explained due to the unexpected factors, e.g. hydrochemistry, or some stochastic processes. It implies that specific micro-distributions of species among the drips are related to specific environmental parameters.
Isolation and 16S rRNA gene sequence analysis of Actinomycetes from weathered rocks in Heshang Cave, central China
MAN Baiying, CHENG Xiaoyu, WANG Hongmei, YUN Yuan, ZHONG Yuhong
2017, 36(4): 572-579. doi: 10.11932/karst20170420
Abstract:
The specific goal of this work was to investigate the actinobacterial diversity in the weathered rocks by culture-dependent approach in Heshang Cave, Hubei, China. Three weathered rocks samples (W1, W2 and W3) were collected from aphotic zone and twilight zone in Heshang Cave with sterile centrifuge tubes in August, 2015. Five modified media and one self-designed medium of extracting of weathered rocks agar medium were used for isolation of actinomycetes in the weathered rocks of Heshang Cave. The isolates were identified by 16S rRNA gene sequencing using special primer for actinomycetes. Result shows that in total of 72 strains obtained by pure culture from 6 different media. The phylogenetic analysis showed that 72 actinomycetes sequences were classified into four genera in three orders of Actinobacteria with Streptomyces being dominative. The number of isolated strains in genera Streptomyces, Rhodococcus, Tsukamurella and Microbacterium was 69, 1, 1 and 1, respectively. Samples of W1 and W2 in aphotic zone were only isolated 9 and 10 strains respectively, while sample of W3 in twilight zone were obtained 53 strains. The results offer valuable information and isolates for the subsequent study on the interaction between carbonate and microbes.
Variations in deposition rate of sedimentary cycle from a stalagmite in Lianhua -Cave and its paleoclimatic implications during the mid-late Holocene
ZHANG Huiling, YU Kefu, ZHAO Jianxin, FENG Yuexing, LIN Yushi, ZHOU Wei, LIU Guohui
2017, 36(4): 580-590. doi: 10.11932/karst20170421
Abstract:
Deposition rate of sedimentary cycle of stalagmite,which is calculated based on 230Th age dating according to sedimentary cycle of stalagmite, is an important parameter of stalagmite formation and an effective paleoclimatic index to reconstruct paleoclimate. Variations in deposition rate of sedimentary cycle may reflect the change of surface temperature and rainfall, which immediately relates to intensity of summer monsoon. Making use of stalagmite LH2, collected from Lianhua Cave, Hunan Province , China, the paper reconstructs the history of surface temperature and rainfall since 8.6 ka BP based on 42 230Th ages. From 8.6 ka BP to 4.2 ka BP, the climate is characterized by high temperature and rainy, the summer monsoon is strong, deposition rate of sedimentary cycle is high. But the climate is not stable and there is a series of millennial to centennial fluctuations.From 4.2 ka BP to now, the climate is cool and dry, deposition rate of sedimentary cycle is low. Generally speaking, in orbital timescale, there is a negative correlation between deposition rate of sedimentary cycle andδ18O record from stalagmite LH2. The deposition rate of sedimentary cycle stalagmite D4 from Dongge Cave duplicates that of stalagmite LH2, which confirms the validity of deposition rate of sedimentary cycle to record climate changes. Basically, changes of deposition rate of stalagmite are controlled by the summer solar radiation in Northern Hemisphere and ITCZ exerts directly influence on it. In centenniarl timescale, deposition rate of sedimentary cycle of stalagmite LH2 may relate to weak monsoon events occuring in the mid-late Holocene.
Environmental changes and their cause of the Zhijin cave in Guizhou Province
YIN Chao, ZHOU Zhongfa, PAN Yanxi, ZHANG Jie, CAO Mingda, ZHANG Shaoyun
2017, 36(4): 591-597. doi: 10.11932/karst20170422
Abstract:
The Zhijin cave is located in the northeast of Zhijin county in western Guizhou Province. The area of Zhijin cave world geological park is 307 km2, and its central scenic spot lies at the intersection of the Liuchong river and Sancha river, where developed the Huangchun dam (T1y2) Formation of Lower Triassic Yelang Group (T1y). Because of the magnificent and unique landscape, the Zhijin cave has been honored with national geological park in 2004 and the world geological park in 2015. From January 2015 to May 2016, monthly monitoring has been conducted to the temperature, air CO2 concentration, air pressure, air humidity and wind speed in this cave. The cave air CO2 concentration was measured by Telaire7001 portable infrared CO2 instrument, of which the resolution and the range are 1 ppm and t 0-10,000 ppm, respectively. The humidity, temperature, air pressure of cave air and wind speed in the tunnel were observed by the Kestrel4500 anemometer. The data on visitor amount are provided by the Zhijin Cave Management Bureau. The previous research data are collected from the literature and compared with the new monitoring data point by point. Then this work analyzes the change of the environment and the number of tourists from the initial stage of opening of the Zhijin cave to the present and the relationship between the environment and the visitor amount and the influence of artificial light sources on the environment inside the cave. Thus the impact of human activities on environmental factors in the cave are quantified, and the main factors affecting the environment inside the cave are identified, which could provide a scientific basis for protection of the cave environment and landscape. The results show that the CO2 concentration and temperature level have been increased significantly since the initial stage of opening of the Zhijin cave, with amplitudes reaching 1,000 ppm and 2-3 ℃, respectively. The maximum CO2 difference was up to 465 ppm between 2011-2013 and 2015-2016. The main factors of the environmental change are tourism activities and artificial light. The amount of tourists has increased from less than 50 thousand in 1985 to 594.571 thousand in 2015, leading to increase of the CO2 concentration with time. The annual temperature difference was not large, but the overall trend was still decreasing year by year and the gap of humidity was not obviously except 2011. The maximum temperature difference between surrounding environment and artificial lights can reach 33 ℃, and the maximum humidity difference between the cave interior and surrounding environment is up to 66.7%.