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2015 Vol. 34, No. 4

Display Method:
In-situ treatment of micro-polluted water supply in natural wells of karst areas
ZOU Sheng-zhang, ZHU Dan-ni, LI Lu-juan, LU Hai-ping, ZHOU Chang-song
2015, 34(4): 309-313. doi: 10.11932/karst20150401
Abstract:
In the regions of Southwest China, natural karstic wells are the main sources for local water supplies in a distributed manner. In this paper, a study on the technical principle of water treatment for some representative karst wells in the karst areas was conducted, based on the analysis of the well water pollution characteristics. The objective of this study is to provide treatment measures for preventing the water from pollutions by any means. In combination of the technical principle with a pilot test, this paper presents in detail the idea for the design and associated design parameters, the technics of water treatment and the matters need attentions during the construction of rapid infiltration tank. Moreover, results of the test showed that, after the treatment of the contaminated well water, its turbidity was less than 5 degrees; the removal rate of trace organic matters reached more than 35%; the ammonia, nitrite and nitrate levels were reduced by more than 60%; and the maximum rate of bacteria removal reached 95% as well. The rapid infiltration technology applied in the water treatment does not require additional chemical agent, thus avoiding any possible adverse effect and hygienic problem arose from the use of coagulant and sterilant. The water quality of the treated natural karstic wells was hence improved, which generally meets the requirements of the national drinking water standards.
Patterns of karst geomorphologic combinations in areas with rich groundwater
WANG Yu, WANG Zi-wei
2015, 34(4): 314-324. doi: 10.11932/karst20150402
Abstract:
Only in rock masses with strong karstification and active karst development, it is possible to form areas with rich karst groundwater or zones with concentrated flows. Karst landform with particular surficial appearance is the result of geological activities controlled by many geological factors such as geological conditions, endogenic and exogenic geological dynamic processes, and neotectonic movements as well. The karst geomorphologic patterns, with the combination of various geomorphologic units, are usually the ground manifestations of underground features and processes such as the formation and evolution of underground karsts and associated groundwater flow and storage. These geomorphologic patterns can accordingly be used as important indicators for identifying the areas that enrich in groundwater resources. In this article, eight karst geomorphologic patterns are presented through the analysis of the information of regional hydrogeological survey and relevant database. For groundwater prospecting and borehole siting purpose, these geomorphologic combination forms that reflect areas of good aquifers are of great value and can provide a great amount of effective information in the hydrogeological survey and drilling. These eight karst geomorphologic combination forms include the sedimentary plain in the karst fault basin or valley, the paleochannel in karst valley and lower land, the isolated karst hill at the valley mouth, the junction of karst valleys, the long belt under the karst fault escarpment, the area of the opposite concave bank in karst valley, the zone with gentle slope and shallow depression, and the karst shallow hill and roomy ridge. In the article, the morphological characters of each karst geomorphologic patterns are also described in detail. Via typical case study, the formation mechanisms of groundwater dynamics in these areas are further analyzed.
Organochlorine and organophosphorus pesticide residuals in the top soils from typical orchards and their risk evaluation in the Lijiang River watershed
XIE Yun-qiu, CHEN Yu, TANG Xiu-guan
2015, 34(4): 325-330. doi: 10.11932/karst20150403
Abstract:
This paper studies the residual pesticides in orchard soils in the catchment of Lijiang River, with the intention of providing valuable suggestions for the development of Guilin International Tourist Resort.The surface soils from the vineyard, the citrus orchard and the peach garden in the Lijiang watershed were sampled to analyze the residual levels of 27 kinds of organochlorine pesticides (OCPs) and organophosphorus pesticides (OPPs). With the method of time succession sequence instead of spatial sequence ,their risks were assessed by using maximum residual limits (MRLs) in Environmental Quality Standard for Soils (GB15618-1995) and Farmland Environmental Quality Evaluation Standard for Edible Agricultural Products(HJ 332-2006), as well as extraneous maximum residue limits(EMRLs) in National Food Safety Standard-Maximum Residue Limits for Pesticides in Food(GB2763-2014). The results show that the concentrations of all 6 OPPs, including methamidophos ,acephate ,dipterex ,dimethoate ,parathion-methyl and malathion, fall below the reported limit ranges; and alike case occurs in 16 out of 21 OCPs analyzed, including toxaphene, atrazine, alachlor,hexachlorobenzene (HCB), alpha-hexachlorocyclohexane (α-HCH), gamma-hexachlorocyclohexane (γ-HCH), delta-hexachlorocyclohexane (δ-HCH), heptachlor, heptachlorepoxide, aldrin, α-chlordane, γ-chlordane, dieldrin, endrin, o,p-DDT, and p,p-DDD. The contents of Dichlorodiphenyltrichloroethane(DDTs),p,p-DDE,p,p-DDT, hexachlorocyclohexane(HCHs) and beta-hexachlorocyclohexane (β-HCH) are below the range of 0.50-10.67 ng/g, 0.50-8.32 ng/g, 0.70-2.35 ng/g, 0.50-0.64 ng/g and 0.50-0.64 ng/g, respectively, with point detection percentages of 68.8%, 68.8%, 6.3%, 6.3% , 6.3%, which are originated from historic usage of the chemical DDT and HCH. The detection percentages are 33%, 25% and 100% for DDTs and 0%, 0% and 6.3% for HCHs in the peach garden and the vineyard and the citrus orchard, respectively. On the basis of topsoil OCPs and OPPs residual levels and according to the soil environmental quality standard GB15618-1995, the soils in three orchards reach the first class which is suitable for the cultivation of safe agricultural products such as citrus, grape, peach and etc.in the Lijiang area.
Preliminary study on contaminant of polycyclic aromatic hydrocarbons in vulnerable karst aquifer in a heavy industry district
KONG Xiang-sheng, MIAO Ying, LUAN Ri-jian, YANG Qi-yong, QIN Su-ni
2015, 34(4): 331-340. doi: 10.11932/karst20150404
Abstract:
One heavy industry district (steel and fertilizer plants) in the karst area of southwestern China was selected as the study area. The groundwater and soil samples in the hydrogeological units were collected, from which 16 polycyclic aromatic hydrocarbons (PAHs) prioritised by USEPA were analysed using GC/MS method. The results show that total concentration of the PAHs in groundwater ranges from 1135.79 to 1361.26 ng/L, with dominant species as phenanthrene, anthracene, naphthalene, chrysene and pyrene. Compared with other regions, groundwater pollution due to the PAHs in the study area is of a middle level. According to National Recommended Water Quality Standards of priority toxic pollutants (2009 USEPA),it is found that benzo[a]anthracene, chrysene, benzo[b]fluoranthene, and benzo[k]fluoranthene exceed the standard. The figures of PAHs characteristic ratio suggest that the PAHs sources in the karst aquifer were derived from incompletely burning and coking of coal, which are similar to contaminant sources discharged by steel and fertilizer plants. The karstic groundwater in the downstream areas have been highly polluted; and it appears that the PAHs concentration in the discharge area is a higher than that of runoff area. Impact of the PHAs on the karst aquifers is sever, which can be attributed to the following two aspects. On the one hand, common presence of karstic depressions, dense fissures developed in the karst, weathered dolomite and fault fracture zones provides a favorable condition for PAHs migration in the karst aquifers which are high vulnerable to the contaminant. Meanwhile, large quantity of groundwater in source areas has been extracted for industrial use, which speeds up the infiltration of pollutants into the karst aquifers. On the other hand, the surface water level in the study area has been raised owing to the construction of the Honghua hydropower station dam which stores huge amount of water in the reservoir; this in turn elevates the groundwater level and slows down its discharge to the stream system. As a result, the self-purification ability of PAHs in the karst aquifer decreases. The location of pollution sources in the groundwater system is also one of the factors that impact of the PAHs migration in karst aquifer. Risk assessment of groundwater suggests that the content of phenanthrene, anthracene, pyrene, benzo[a]anthracene and benzo[b]fluoranthene in the karst groundwater is at a very high risk grade. Thus, it is suggested that local government should take immediate intervention to reduce this pollution risk.
Chaos analysis and prediction of monthly runoff time series in the Nandong subterranean river
QIN Xing-ming, JIANG Zhong-cheng, LAN Fu-ning, Ma Zu-lu, ZHAO Yi
2015, 34(4): 341-347. doi: 10.11932/karst20150405
Abstract:
In order to provide scientific evidence for the development and utilization of water resources in the Nandong area,this study analyzes the nonlinear features of monthly runoff series of the subterranean river from 1990 to 2013. It is based on the phase space reconstruction theory and chaos theory. The optimal embedding dimension and time delay for the real monthly runoff series are determined using the improved false nearest neighbor method and mutual information method,respectively. And the saturation correlation dimension and the largest Lyapunov exponent for the series are calculated to distinguish its chaotic characteristics by using the Grassberger-Procaccia method and small data sets. According to Volterra series theory,a prediction model is established to describe the changes of monthly runoff series of the Nandong subterranean River in the future. The results show that the time delay and optimal embedding dimension τ=5 and m=8, respectively. The saturation correlation dimension of attractor of phase space is 4.63 and the maximum Lyapunov index is 0.748 9. The results also indicate that the monthly runoff series in the Nandong subterranean river has a weak chaotic characteristic in both quality and quantity. The model using the third-order Volterra adaptive filter is effective to predict hydrologic chaotic time series in the study area. It is accurate enough for monthly precipitation forecasting,especially for short-term precipitation forecasting within 18 months.
Characteristics of heavy metal element distribution in the groundwater system of typical karst regions: A case study in Poyue underground river, Guangxi, China
DU Yu-chao, PEI Jiang-guo, LU Li, LIN Yong-sheng, Fan Lian-jie
2015, 34(4): 348-353. doi: 10.11932/karst20150406
Abstract:
Underground river is an important part of karst groundwater system. The purpose of this work is to reveal the concentrations and spatial variation of heavy metals represented by zinc (as Zn), aluminum (as Al) and Manganese (as Mn), in particular by the five toxic heavy metals, under the typically hydrogeochemical environment in the Poyue underground river system, Guangxi. Water sample were collected at the localities along defined cross section lines in the field and the concentrations of heavy metals were analyzed in laboratory. The results show that pH value of the Poyue groundwater is between 7.34 and 8.10, with an average of 7.67. Toxic heavy metals detected in the underground river have very low concentrations, much less than the level of III water quality category recommended by the national environmental quality standards. Therefore, the karst groundwater is suitable for a variety of purposes. The results also show that higher concentrations of these elements occur at the localities where the underground river exposes on the surface or surface water in the recharge area, with the maximum values at the underground river outlet located at slope toe. The reason is that in the slope area, industrial, agricultural and mining activities are extremely strong, which is characterized by the dumps of industrial and mine (such as gold mine) tailing wastes on the slope. This causes the occurrence of the heavy metals in the karst river system.
Comparison of the REKST model with PLEIK model in performing the antifouling analysis of karstic groundwater :A case study in the Xiangxi Dalongdong underground river
DAI Chang-hua, LI Hai-bing, PAN Zhuo, ZHAO Shuai-jun, HUANG Shu-chun
2015, 34(4): 354-361. doi: 10.11932/karst20150406
Abstract:
By taking the Xiangxi Dalongdong underground river as a case study area, this paper comparatively analyzes the performance of the REKST and PlEIK models in anti-fouling evaluation in karstic bare-rock areas. Analytical results show that there is a big gap between these two models in terms of their functionalities, particularly in grading and ranking processes, because in these two models their index assignment and weighting methods are different. The REKST model is lack of quantitative index assignment and barrier property grading systems; while the PLEIK has the both, so that the effect of subjective factors on results for PLELK are small. Thus, the PLEIK model is superior to the REKST model in the assessment.
A study on the pollution boundary of karst groundwater system and its antifouling performance in Dabanqiao, Kunming
PENG Shu-hui, WANG Yu, HUANG Cheng, LI Qin, WANG Yu-qin
2015, 34(4): 362-368. doi: 10.11932/karst20150408
Abstract:
The Dabanqiao karst groundwater system is located at some 17 km in the east suburb of Kunming. The area belongs to subtropical plateau monsoon climate, characterised by four spring-like seasons, uneven distribution of annual rainfall, and distinct dry and wet periods. The Baoxiang river is the primary surface drainage in this system.The area extends from the northeast to the southwest. Its north and northeast are dominated by medium to low solution mountains composed of carbonate rocks, while the southwest is a sedimentary plain with flat terrain and sporadic erosion/solution monadnock.The karst aquifer system in the area mainly consists of P1y carbonate rocks. The P2e basalt, P1l clastic rocks and faults jointly constitute the impervious boundary of the system. The strikes of geological structures in the system are mainly in the direction of northwest, northeast, and north-south.This study is conducted on the basis of the geological survey project commissioned by Ministry of Land and Resources, as well as comprehensive analysis of existing results and field investigations. The objective of the study is to find out the pollution boundary of the karst groundwater system through the research of typical karst groundwater system in the Dabanqiao area; furthermore, to gain a better understanding of the karst water pollution-proof property and to lay a concrete basis for the water vulnerability assessment.The groundwater in Dabanqiao area is a typical bare-covered karst groundwater system developed in the fault basins of the eastern Yunnan area. In this paper, the groundwater pollution boundary is identified and the grades of the groundwater system is determined. The results show that the Dabanqiao groundwater system is the first-order , which consists of two subsystems, i.e. the Hengshan-Longquansi bare type subsystem and the Dabanqiao-Adicun covered one.This work determines four types of pollution boundaries ,which are the lateral boundary of the Dabanqiao karst groundwater system, top boundary of the bare area, the boundary between bare subsystem and covered subsystem and the top boundary of the covered area. And we also study the antifouling performance of the boundaries. The results show that the antifouling performance of the bare area top boundary is weak,that of the boundary between bare subsystem and covered subsystem is relatively weaker and the antifouling performance is better on top of the covered area. Through this study we can gain a better understanding of the contanmination-proof ability of the bare-covered karst groundwater system and lay an environmental hydrogeology foundation for calculating and evaluating the vulnerability of groundwater due to contamination using the model of the karst groundwater system.
Distribution characteristics and influence factors of the ammonia, nitrite and nitrate in the Lijiang River, Guilin City
SHEN Hao-yong, JIANG Guang-hui, GUO Fang, GUO Xiao-jiao
2015, 34(4): 369-374. doi: 10.11932/karst20150409
Abstract:
The Lijiang River, an internationally famous karst scenic area, is the main source for massive water supply to Guilin City. It is reported that ammonia is one of three major nitrogenous contaminants, according to the monitoring data derived from 962 water stream sections in ten first catchments across China. To determine the temporal and spatial distribution characteristics of ammonia-nitrite-nitrate and associated influential factors, 7 sections on the Lijiang River and its tributaries are selected. The samples of surface water were collected during the wet and dry seasons, respectively. The analytical results of field chemical/physical parameters and laboratory experiments show that the highest concentrations of NH3-N and NO3--N are 0.248 3 mg/L and 2.251 7 mg/L, respectively, which fall in the range of gradeⅡwater recommended by the national environmental surface water quality standards. The concentration of NO3--N is also below the limit requirement of surface water sources for collective drinking water supply. However, the results also show that the ammonia-nitrite-nitrate concentrations in the Lijiang River have increased by various degrees and the water has a tendency of deterioration after the river flows through the Guilin City. The temporal distribution characteristics of ammonia-nitrite-nitrate is that the concentrations of NH3-N and NO3--N are higher during dry seasons and the concentration of NO2--N becomes higher during wet seasons, The ratio of C(NH3-N)/ C(TIN) is 4.83% in wet seasons; and the figure rises to 6.69% in dry seasons because of temperature change. The increasing of ammonia nitrite and nitrate nitrogen is attributed to the additional pollutants contributed from the tributaries of the river such as Xiaodongjiang river and Taohuajiang river, which are flowing through the rural domestic and agricultural area where is lack of sanitation facilities. In addition, the concentration of NH3-N has a raising trend and the concentration of NO2--N and NO3--N is almost steady when it rains or during flood seasons because of agricultural non-point sources. Therefore, it is necessary to control and manage the contaminant inflow from the tributaries of the Lijiang River in a comprehensive manner and develop a real-time network to monitor the water sources area, especially monitor the NH3-N concentration fluctuation in rainy season.
Current situation of groundwater organic pollution and control measures in Guanshanhu Lake to Baiyun areas, Guiyang City
YANG Xiu-li, LUO Wei, ZOU Sheng-zhang, NING Li-yuan, ZHU Xue-shu
2015, 34(4): 375-381. doi: 10.11932/karst20150410
Abstract:
The research area is situated in the typical exposed-covered karst area in central Guizhou hilly plain of the Guizhou plateau, where many karst underground rivers and springs have been developed, which is indicative of abundant groundwater resources. In order to clarify the organic pollution status and distribution characteristics in the groundwater, 43 representative sites were selected and water samples were collected both in dry and rainy seasons to analyze organic components, on the basis of the classification of 12 groundwater systems and the potential pollution sources in each groundwater system. The results show that 32 of 86 samples contain organic contaminants. The concentrations of 10 organic pollutants out of 27 organic components analysed are above recommended limits. The pollutant detected ratio of chloroform is the highest with a value of 29.07%, while the ratios of other organic components are lower than 5%, except for one sample with dichloropropane level exceeding the standard. The organic pollutants are detected in 9 groundwater systems, where the contamination sources are mostly located in vicinity of the waste discharges from industries and mines especially from medium-to small-scale enterprises, and some streams and trenchs that divert contaminated substances as well. These pollutants reach groundwater in a concentrated infiltration way through karstic conduits such as sinkholes and karst windows. In overall, the detected ratio of the organic pollutants is relatively high but most of their concentrations are below the national standards; the groundwater in this area is slightly polluted. To prevent the water from further deterioration, it is necessary to implement integrated water management measures via controlling the pollution sources in medium-to small-scale industries, accelerating the construction of pipeline network for industrial and domestic wastewater and improving the pollution monitoring network.
Significance of paleokarst water supply developed in Maokou Formation in western Guizhou
CHEN Ping
2015, 34(4): 382-386. doi: 10.11932/karst201505y03
Abstract:
For strong surface cutting, it is in poor groundwater occurrence and barren enrichment, and the shallow aquifer is almost no water in the west of Guizhou, where it is engineering water shortage. The water supply problem in the west should be solved urgently.The Paleokarst developed in Maokou formation of Permian in Guizhou is proved to be a good space for the deep buried groundwater occurrence and migration, which combines the overlying strata to be a deeply buried ground water system with abundant water in the control with good geology and geography . Based on the exploration experimental data, the development of the paleokarst and reservoir characteristics were studied in Maokou formation of Permian of the basalt and siliceous rocks covered areas in western Guizhou .Through the comprehensive analysis, the results show that top paleokarst commonly develop in Maokou formation, which is generally made of karstic fissure. Besides, karst is most concentrated along the fault zone, where groundwater is most concentrated and permeated. Emei mountain basalt area and Maokou paleokarst belt constitute a good “closed-buried” type of reservoir structure, being the important targets of finding the water source to guarantee drinking water security in western Guizhou.
The pollutant infiltration pathways and measures to control groundwater pollution in the Guijiang River drainage system
HE Yuan, ZHANG Ying, ZHU Ming
2015, 34(4): 387-394. doi: 10.11932/karst20150412
Abstract:
The investigation of karstic groundwater pollution in areas of Guijiang River has recently been completed; and our research findings show that the pollution sources can basically be categorized into nitrogenous, heavy metal and organic compounds. Among them the nitrogenous (nitrite, nitrate and ammonia) pollutants were mainly derived from industrial activity, livestock farming, domestic sewage and waste and the use of nitrogenous fertilizers, while heavy metal pollutions are attributed to industrial and mining activities and organic compounds to the impact of industries and livestock farming. In this case, the patterns of pollutants that migrate downward to reach the karst groundwater include diffuse and concentrated infiltrations, of which the former usually happens at isolated peak karst plains , rocky hill karst valleys. Concentrated infiltrations largely take place at the sink points in isolated-peak karst plain,the ponors in peak-cluster depressions and karst windows in peak-cluster and hoodookarst valleys. Systematic tests and analyses were performed to evaluate the rate of groundwater pollution. Results show that nitrogenous pollutions occur in 36.5% of the water samples which are broadly distributed over the karst autogenic recharge area in a diffuse infiltration manner. In the meantime, heavy metals in 15.3% water samples are above the directives of water quality regulations; and these point pollution sources enter groundwater via concentrated infiltration largely happens at the localities as sink points and ponors in peak-cluster poljes and via diffuse infiltration in the karst valleys. As heavy metals are easily absorbed by sediments, karst groundwater around the pollution sources has been more likely contaminated. Organic compounds were detected in 3.49% of the water samples, which are distributed at the downstream of the alluvial plain; and the pollutants that infiltrate into groundwater demonstrate a feature of short linear or point pollution because of the low hydraulic gradients of the groundwater.
Characteristics of pollution of the Chaoyangxi river to groundwater in Nanning of Guangxi
LU Hai-ping, KONG Xiang-sheng, ZOU Sheng-zhang, MIAO Ying, LI Lu-juan
2015, 34(4): 395-401. doi: 10.11932/karst20150413
Abstract:
Rivers in urban and suburban areas, which often become sewage ditches, are the key reason of the deterioration of urban water environment and ecosystem. The Chaoyangxi river is located in Xixiangtang district, north of Nanning City. As it has long used as a waste receptor without timely treatment, large amount of heavy metals and organic sludges are suspended in the water and deposited on channel bed. This river, with water characterised by black color, very unfavorable odor and high phosphorus and high heavy metal contents, is one of the most seriously polluted inland rivers and the famous stinking ditch in Nanning.The study area is located in the Lianchou village of Beihu Industrial Park in the upstream of the Chaoyangxi river, where the grade II terrace has been developed in northern side of the river. The objective of this study is to look at the influence of urban sewage on the shallow groundwater. The aquifer with high permeability largely comprises round gravels of the Quaternary period. There are a lot of sewage outlets in the upper reaches and surrounding areas of the river. The discharge of urban sewage and wastewater is the main artificial recharge and pollution source. The continuous discharge and fast infiltration of the sewage water into the aquifer has caused sever pollution of the shallow groundwater.This paper analyzes pollution characteristics of the sewage ditches in the vicinity of the shallow aquifer, by using the monitoring data derived from 5 boreholes and 3 wells with a main focus on the organic substances such as three major nitrogenous compounds (ammonia, nitrite and nitrate, hereafter as ammonia nitrogen), polycyclic aromatic hydrocarbons (PAHs) and organochlorine. The results show that the sewage ditch produces obvious pollution to the shallow groundwater where the ammonia nitrogen concentration in the river water reaches 42.05 mg/L. Meanwhile, 6 out of 8 groundwater samples have an ammonia nitrogen level in excess of the groundwater quality standard by 1 to 65.75 times. The degree of groundwater pollution in industrial area is lower than that of agricultural and wasteland area. The reason is that during the building construction in the industrial area, the gravel layer has been excavated and heavily compacted for building foundation purpose; this has caused the reduction of the shallow aquifer's permeability and retarded even blocked the infiltration of pollutants.The pollution degree gradually decreases along with the increasing distance from the contaminated groundwater body; and it fluctuates seasonally. In high-water period, the pollution degree is significantly lower than that of low-water period. The major sources of ammonia nitrogen are the domestic and livestock waste directly discharged into the Chaoyangxi river. The main pollution sources of PAHs are from the combustion of grass, wood and coal. DDT pollution is derived from historical pesticide residue and the presence of BHCs can be attributed to the use of lindane in the upstream and remote atmospheric drop.
Cd2+adsorption characteristics of typical soils in karst areas
ZHU Dan-ni, ZOU Sheng-zhang, ZHOU Chang-song, LI Lu-juan, LU Hai-ping
2015, 34(4): 402-409. doi: 10.11932/karst20150414
Abstract:
The problem of cadmium (as Cd and Cd2+)pollution is prominent in karst areas. This paper studies it adsorption property to reveal the migration of Cd2+in the soil environment, thus providing a scientific basis for the environmental risk assessment of the soils. Adsorption of Cd2+by calcareous soils (brown calcareous soil、black calcareous soil) in the karst areas was investigated via batch sorption experiments. The results show a higher sorption capacity of calcareous soil to the heavy metal Cd, with the mean adsorption rate ranging from 89.84 to 98.84, of which black calcareous soil is greater than that of brown calcareous soil. The isothermal adsorption process of the both calcareous soils can be satisfactorily described by Langmuir and Freundlich models, while simulative result of the latter is better than that of the former. In the meantime, the Elovich,two-coefficient,W-M and first-order models are used to simulate the soil Cd2+sorption kinetics. On the one hand, the Elovich and two-coefficient equayions represent the best models to simulate the adsorption kinetics of Cd2+in brown calcareous soil with the correlation coefficients in excess of 0.9.On the other hand, the adsorption kinetics of Cd2+in black calcareous soils only fits the Elovich,two-coefficient and W-M equations with the significance level of above 0.8. The simulations for the black calcareous are processed with an initial Cd concentration of 100 mg/L, where the Elovich model is proved to be the best one. Moreover, the soil property analyses show that the contents of organic matters, calcium carbonate and CEC have a significant impact on the adsorption capacities of the soils studied, while the contents of iron, aluminum and silicon oxides in the soils show a minor influence on their Cd absorption capacities.
Characteristics of the content and distribution of heavy metals in groundwater in Mashan area, middle to lower Hongshui River, Guangxi, China
FAN Lian-jie, PEI Jian-guo, DU Yu-chao, LU Li, LIN Yong-sheng
2015, 34(4): 410-414. doi: 10.11932/karst20150415
Abstract:
Based on the groundwater data obtained from the karst groundwater and information gained from the groundwater pollution investigation and evaluation in the southwest China, this work analyzes geochemical characteristics of 10 heavy metals with 27 karst groundwater samples collected in Mashan area located in the middle to lower Honghe River. The main focus of this study is to establish a relationship between the concentrations of heavy metals and their spatial distribution and the other chemical constituents dissolved in the karst groundwater, as well as the relationship between the heavy metals studied. The results indicate that the concentration of heavy metals is lower than the upper limit for drinking water standard of China, and the contents of heavy metals in the groundwater follows a descending order as Fe>Al>Zn>Mn>Pb>Se>As>Cd. There is a remarkably positive correlation between Mn, Fe, As and Al, and a significant positive correlation between Zn and Pb, Cd in the groundwater as well. The relationship between Se and other seven heavy metals is not that apparent, perhaps due to the diversity of the heavy metal sources. All the heavy elements have no correlation with pH, whereas the chemical contents HCO3-, Ca2+and HCO3-have a great impact on the heavy metal concentrations. TDS has little effect on most of the heavy metals, but a certain effect on the appearance of As and Cd. In terms of spatial distribution of the heavy metals, the localities with high concentrations mainly occur in and around the city Mashan and townships in the vicinity of Guzhai and Qiaolijie.
R mode analysis for influencing factors of karst groundwater quality in middle and upper reaches of the Hongshuihe river
LU Li, WANG Zhe, PEI Jian-guo, DU Yu-chao, LIN Yong-sheng, FAN Lian-jie
2015, 34(4): 415-419. doi: 10.11932/karst20150416
Abstract:
To control and manage for groundwater contamination in the middle and upper reaches of the Hongshuihe river, Rmode factor analysis was conducted on 130 samples from this area. Three main factors which affect the quality of karst groundwater are recognized in study area. The first main factor is dominated by Ca2+, HCO3- , total hardness and total dissolved solids, which shows the water-rock interaction. The second factor is made up of K++Na+, Cl- and NO3-, which reflects agricultural pollution and domestic wastewater in the agricultural area, such as pesticide, fertilizer, and animal waste. The third factor is composed of Mg2+, SO42-and F-, which reflects industrial and mining pollution in the northern mine area. The results show that these three factors are closely related to human activities, which would be monitored and controlled more strictly in the future.