• Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology

2010 Vol. 29, No. 1

Display Method:
Laboratory simulation on soil erosion under different bedrock outcrop ratein Southwest karst area, China
WANG Ji, CAI Xiongfei, LEI Li, ZHANG Hao
2010, 29(1): 1-5. doi: 10.3969/j.issn.1001-4810.2010.01.001
Abstract:
This paper chooses Southwest China karst area as the research region. On the basis of data analysis and field research work, a rain-simulator is designed, which could fulfill the range of rainfall intensity in this area. Twelve processes of soil erosion simulation are made on the slopes with different gradient under different bedrock outcrop rate. Results of the simulation are as follows: (1) The slopes runoff ratio keeps steady after 180~300 s and hardly changes with the increase of gradient. (2) The change trend of transport rate of sediment yield can be divided into five periods: rapid increase, decrease, increase, slow decrease and steady. The transport rate of sediment yield decreases with the increase of the bedrock outcrop rate on same or different slopes, and the changing extent decreases by 40.2% to 1.0% with the increase the of slope. (3) The total sediment yield decreases with the increase of the bedrock outcrop rate on same or different slopes, and the changing extent decreases with the increase of the slope.
Spatial heterogeneity of soil moisture under different vegetation types in peak-cluster depression
SONG Tong-qing, PENG Wan-xia, ZENG Fu-ping, LIU Lu, DU Hu, LU Shi-yang, YIN Qing-cang
2010, 29(1): 6-11. doi: 10.3969/j.issn.1001-4810.2010.01.002
Abstract:
In this paper, the authors tries to illustrate the spatial heterogeneity of the soil moisture in surface layer (0~10 cm) under four typical vegetation types and the ecological processes and mechanism in peak-cluster depression. The results show that the soil moisture in surface layer increases significantly with the reduced disturbance gradient, and vegetation takes a succession change from crops (Ⅰ) to man-made forest (Ⅱ), to secondary forest (Ⅲ), to primary forest (Ⅳ). The spatial heterogeneity of the soil moisture in surface layer under the four vegetation types is diverse. Exponential, Gaussian, exponential and spherical models fit best for the spatial patterns of soil moisture in surface layer inⅠand Ⅲ, Ⅱ, and Ⅳ, respectively. The values of (C0/ (C0+C)) ranged from 0.269 to 0.500, which indicates the soil moisture in the four types having medium spatial autocorrelation. The spatial patterns of the soil moisture in surface layer are similar in type Ⅰand Ⅳ, with relative large value of (C0/ (C0+C)) and fractal, which suggests less dependence on spatial existed in the two vegetation types. The reverse is true to type Ⅱ and Ⅳ. The range in typeⅠis up to 252.9 m, and the ranges of the other three vegetation types are relative small (from 141.2 to 163.2 m). The Kriging contour maps clearly show the spatial distribution of the soil moisture in type Ⅰ and Ⅳ is convex, while that in Ⅱ is unimodal and in Ⅲ concave. It is suggested that spatial pattern of the soil moisture in surface layer is affected by a large number of factors, among which disturbance plays a key role through regulating vegetation. Therefore, to reduce disturbance might be an important measure for the improvement of water resource and the restoration of eco-environment in karst peak-cluster depression.
Optimized allocation for land use and resources use in north Guangdong karst area
LIAO Yi-shan, ZHUO Mu-ning, LI Ding-qiang, CAI Qiang-guo, GUO Tai-long, CHEN Xin-jiao
2010, 29(1): 12-19. doi: 10.3969/j.issn.1001-4810.2010.01.003
Abstract:
Xiushui small watershed, a typical rocky desertification area in north Guangdong Province, is chosen as an example to research the land resources for optimizing the layout and countermeasures under different space-time scales in this paper. The results show that (1) Water is seriously short in the area. The area of land with low, middle and high soil moisture account for 79.94%、10.72%、9.35% respectively, which corresponding to <4.702, 4.702~8.05 and >8.05 in topographic index . (2) Slope land is the most important arable land in Xiushui small watershed. The landuse style should be allocated as follows: contouring farming or covering farming be adopted if the gradient is <10°; plant hedge be adopted if the gradient is 10°to 25°; reforest if the gradient >25°. On the other hand, as the altitude and irrigation affecting the crop, the farmland between 400 to 500 m in elevation is suitable for maize. In the area without irrigation, high water consumption crop should be planted in first half year and maize or other drought-enduring crop planted in second half year because there is more rainfall in first half year but little rainfall in second half year.
Relationship between soil erosion and rocky desertification in Southwest China karst region-A case in Nanchuan karst area, Chongqing
WEI Xing-ping, YUAN Dao-xian, XIE Shi-you
2010, 29(1): 20-26. doi: 10.3969/j.issn.1001-4810.2010.01.004
Abstract:
The paper takes Nanchuan in Chongqing as an example and obtains change relationship between soil erosion intensity and rocky desertification via TM remote sensing image and Arcgis as well as Erdas software on the basis of map algebra principle to transfer matrix of image data. The results show that the increased area of soil erosion is 9 605.89 hm2 and the decreased area is 79 947.85 hm2 from 1988 to 2000 while the increased area of rocky desertification is 15 078.92 hm2 and the decreased area is 12 492.53 hm2. Rocky desertification is a result of long-term effect of soil erosion and soil erosion is the stage of rocky desertification, i.e. there is causal relationship between them. But the area of rocky desertification lightening lags that of soil erosion. The reason for the lag is that the time for ecological restoration of the rocky desertification is longer than that for soil erosion.
Discussion on the soil erosion problem caused by coal-mining and the countermeasure in Guizhou karst mountain
ZHOU Guo-fu
2010, 29(1): 27-31. doi: 10.3969/j.issn.1001-4810.2010.01.005
Abstract:
Coal resource is abundant and coal mining is very active in Guizhou province. According to the statistics, the proven reserve of coal is 50 billion tons in Guizhou. There are 2143 coal mine in Guizhou,2005,and township small coal mine is more than 1 700. Coal mining, occupying land very common, usually causes serious soil erosion. Among them, only the coal mine integration, technological transformation and new project have occupied land and caused soil erosion approximately 250~300 km2 in area in the recent years, which increased more than 1 million tons of soil erosion. Especially, the most serious soil erosion is caused by coal mine construction with the average erosion modulus higher than 7 500 t / a?km2 in most case, even higher than 15 000 t / a ? km2 in individual lot. There are many problems during Guizhou coal mine integration, the existence of the "three simultaneous" may not be implemented, control areas of responsibility defined in unreasonable and inadequate coverage of prevention and control measures, inappropriate species selection, soil prevention and control techniques backward, inadequate investment in water conservation and other issues. So, in order to reinforce more scientific measures in soil and water conservation in the future, soil and water conservation works in coalmine area should be incorporated with regional soil and water conservation project, and scientific research on the relationship between karst environment and soil erosion should be enhanced. Meanwhile, it is needed to expand the scope of responsibility and to increase budgetary unit price in the preparation of the soil and water conservation programme.
On conception of tree planting in karst rocky desertification area——Methods for tree planting by storing water in fracture made by blasting, excavating hole in bedrock
YANG Guang-zhong
2010, 29(1): 32-34. doi: 10.3969/j.issn.1001-4810.2010.01.006
Abstract:
According to the environmental geology and hydro-geological features in karst region, and combining the successful example that digging and planting trees in the shallow dolomite covered areas in Kaili, Guizhou, the author proposed for the first time the idea of tree planting by storing water in fracture made by blasting, excavating hole in bedrock. That is, loosening the rock mass by blasting firstly, then plant trees in the hole by drilling rock and earth up the trees, and using the blasting cystiform gap space to create local groundwater sump to feed water upwards depending on capillary action. And then, the plant roots can grow downward to absorb groundwater and effective nutrient elements, which enable the trees easily being nourished over a long period of time and growing into useful timber even woods. This method is easy to implement, which can be widely used in karst area and other rocky areas. By doing this, expected results of quickly eco-environmental restoration could be achieved.
Changes of soil physicochemical and microbial features during the typical vegetation restoration in karst mountain
REN Wei, XIE Shi-you, XIE De-ti, FENG Hui-fang
2010, 29(1): 35-40. doi: 10.3969/j.issn.1001-4810.2010.01.007
Abstract:
Five types of vegetation(farmland, 1-year abandoned farmland, bush-grass land, 15-year scattered woodland(Platycladus orientalis)and 25-year woodland(Platycladus orientalis))are selected to investigate the changes of soil physicochemical and microbial features during the vegetation restoration in karst mountain. The results show that the soil improving process is complicated. Density increases first and then decreases. The trend of bulk density is just opposite to that of total porosity. Soil available water capacity in bush-grass land is the lowest. The amount of >0.25 mm soil water stable aggregate content has increased by 5.1%~12.5% in the last four stages than that in farmland, and the amount of >0.25 mm soil water stable aggregate content in the bush-grass land is the highest. Aggregate destruction ratio gradually decreases by 34.0%~64.7% from abandoned farmland to woodland with a obviously close correlation with organic matter content. The total nitrogen and available nitrogen have the same increasing trend during the vegetation restoration. The total soil microorganism decreases at first and then increases. The quantity of bacteria group is much higher compared to other two groups at every stages, which accounts for 66.7%~93.3% against the total. The bacteria group is also the most important contributor to soil respiration. The difference for soil characteristic is the result of comprehensive function of surface vegetation composition, litter composition and other different features.
Bryophytes and its heavy metal accumulation in mercury-gold ore belt in the karst area of southeast Guizhou
LIU Rong-xiang, ZHANG Zhao-hui
2010, 29(1): 41-47. doi: 10.3969/j.issn.1001-4810.2010.01.008
Abstract:
The San-Dan (Sandu-Danzhai) Mercury-Gold Ore Belt in the karst area of southeast Guizhou belongs to the Carlin-type mercury-gold deposits. Long-term mercury ore and gold ore exploiting and smelting led to serious environmental pollution in San-Dan Mercury Belt. Based on extensive investigation of the bryophytes in the area, it is discovered that the bryoflora consists of 58 species and 26 genera in 13 families. The dominant families are Bryaceae and Pottiaceae. The concentration of Cd, Pb, Cu, Zn, Ca, Mg, As and Hg in bryophytes and their substrates are measured. Hydrogonium consanguineum, Bryum algovicum, Weisia controversa, Bryum lonchocaulon, Trichostomum crispulum, Haplocladium angustifolium, Entodon aeruginosus and Entodon aeruginosus are the dominant species in Mercury-Gold Belt. The results show that Ca concentration is the highest, Mg the second and the Cd the lowest in the plants of eight main species of bryophytes. Hg-Zn shows prefect correlation at 0.01 level, Hg-Pb shows coefficient at 0.05 leve1, but As-Cd shows negative correlation at 0.05 leve1. Based on the analysis on the accumulation coefficient, all the eight species have ability to accumulate Copper. Weisia controversa and Bryum algovicum could accumulate more than four types of heavy metals. It indicates that these two species have strong tolerance to contamination by Mercury-Gold ore belt and is good materials to be used for bioremediation and comprehensive treatment of abandoned mining site.
Heavy metal content in animal body and its relations with soil and water in the Zhengjia small cave, Guizhou Province
XU Cheng-xiang, LI Dao-hong, MEI Jie
2010, 29(1): 48-53. doi: 10.3969/j.issn.1001-4810.2010.01.009
Abstract:
In this paper, cave animal and heavy metal pollution in Zhengjia small cave in Anshun City, Guizhou Province is studied. The collected samples is 551, belonging to 3 phyla, 6 classes, 10 orders,20 families and 29 groups. The content of heavy metals in 5 groups of animals(snail, diplopod, Diestrammena marmorata ,bat guano and Orthomorpha) and that in the soil and water in cave is determined, and the accumulation coefficient of all animal groups and pollution index of soil in cave is studied. The results show that contents of Zn in bat guano(670.5 mg/kg) is the highest, inferring indirectly the pollution of Zn in the environment around the cave is more serious. Diplopod has not accumulation ability to Ni and Diestrammena marmorata has not accumulation ability to Cr and Ni too. The average contents of all elements in the soil with light belt, dim light belt and dark belt exceed the background value of soil in China, ordering as Zn>Ni>Cu>Cr>Pb>As>Hg>Cd, and Zn>Cr>Ni>Cu>Pb>Hg>As>Cd in water body. The single pollution index shows that Hg, Ni and Zn pollution are severe in the soil, averaging 5.11, 3.18 and 3.02 in light belt, dim light belt and dark belt respectively. The average of comprehensive pollution index (2.17) shows that the pollution is light in light belt, dim light belt and dark belt, which means that this cave has been polluted by heavy metal, but not seriously.
Seasonal variation of copepoda and cladocera communities in subtropic karst reservoir — Case in the Hongfeng, the Baihua and the Aha lakes
CHEN-Chuan, LONG Sheng-xing, REN Qi-fei, MA Jian-rong, WANG San, LI Li, LI Qiu-hua
2010, 29(1): 55-61. doi: 10.3969/j.issn.1001-4810.2010.01.010
Abstract:
Copepida and cladocera community is investigated for four times in the Hongfeng, the Baihua and the Aha lakes from 2008 to 2009. It is found that the copepod consists of 5 families, 11 genera, 19 species with one species is not identified and the cladocera consists of 5 families, 9 genera, and 14 species. Dominant species of copepoda are T.prasinus(Fischer), C.uicinus lobosus Kiefer and T.breuifurcatus Harada. Dominant species of cladocera are D.longispina(O.F.M.), C.cornuta Sars and B.longirostris(O.F.Müller) in all lakes. Total density of copepoda and cladocera is highest in spring, lower in autumn, lowest in summer in both the Hongfeng and the Aha lakes; the highest in summer, lower in autumn, lowest in winter in the Baihua lake. Seasonal biodiversity ordering ranks as AH>BH>HF in spring, BH>AH>HF in summer and winter, and AH>HF>BH in autumn. Seasonal weather change and pollution is important factor affecting copepida and cladocera community change.
Analysis on gushing water in complex karst mining area— A case in ferromanganese mine Ⅱ in Daoxian, Hunan Province
LIN Zhong-xiang, CHEN Xiang-gui
2010, 29(1): 62-69. doi: 10.3969/j.issn.1001-4810.2010.01.011
Abstract:
Water gushing of mine is the most important issue in mining, and reasonable predicting method for gushing water is a hot and difficult problem in research circle at present. Ferromanganese mine Ⅱ in Daoxian, Hunan is taken as the example. The water gushing of mine is simulated by means of finite-difference methods. The simulation results shows that the gushing water mainly comes from the Chezijiang river but the water come from rainfall, the east, south and north boundary increase, which proving the gushing water is recharged widely. On the other hand, the lithology and geological structure as well as groundwater characteristics are investigated, the boundary conditions are determined, and the finite difference numerical methods are used to simulate the groundwater. The results show that, the numerical simulation can be used to forecast water gushing of mine in different conditions and different mining level as well as complex hydrogeologic conditions. In one word, the simulation results can be used as the basis for the design of mining.
Measurement method of recession discharge of karst depression—A case study on Ganjiacao karst depression in Qingmuguan underground river, Chongqing
LUO Jian-yin, YANG Ping-heng, YUAN Dao-xian, LI Yuan-qing
2010, 29(1): 70-74. doi: 10.3969/j.issn.1001-4810.2010.01.012
Abstract:
Recession discharge in submerged karst depression is a special type of pressurized pipe-flow. So, the measurement of the discharge of this pipeline flow is one of major problem in karst hydrology study. The particularity of the pressurized pipe-flow is analyzed and a basic theory and method for inferring the relationship between H and Q is made by means of change in storage capacity of the depression in this paper. And then, method of reservoir inflow under submerged conditions, recession discharge of storage capacity, and total recession discharge under a certain water level is described in detail based on the data from Qingmuguan karst underground river system. In addition, the installation method of field water level monitoring station is introduced briefly in the paper.
Analysis on Leakage and Pollution Prevention Methods of Phosphogypsum Sit in Pingba
ZHENG Wencheng, JIA Hongbiao, GUO Ming, CHEN Ke
2010, 29(1): 75-80. doi: 10.3969/j.issn.1001-4810.2010.01.013
Abstract:
Because of not being done anti-seepage treatment, the leachate containing phosphorus and fluorine produced by the phosphogypsum yard of Pingba enter the surrounding systems of surface water and groundwater though the sewage drains, karst pipes and cracks. The leachate contaminat water of Yangchang River and affected the water environment of Hongfeng Reservoir. In this paper, the development of joint and karst were found out, the hydraulic connection between the surface water and ground water were analyzed, the channel of the leachate flowing into the Yangchang River is 02 aqueduct and the rode from 01 aqueduct and L1 to Q16 and jointed rock mass, the pollution of groundwater subject to jointed surface which main direction is north and west, this were based on the methods of hydro-geological survey and statistical inquiry of quadrat and water-pressure test and connection test. Through the water sample monitor, the scope and extent of water pollution were delimited. Finally, the pollution prevention and control measures such as vertical and horizontal seepage and drainage collection and surface coverage were put out.
Discussion on the impact of karst topography to urban development-A case in Guiyang city
GAO Hong-yan, DIAO Cheng-tai
2010, 29(1): 81-86. doi: 10.3969/j.issn.1001-4810.2010.01.014
Abstract:
Based on the quantitative analysis of surface slope and topographic relief in Guiyang city through DEM data and GIS method, it is pointed out in the paper that karst landform affects Guiyang city’s urban shape, urban construction land supply, road systems and greenbelt system as well as construction cost. Guiyang city has high mountain with abrupt slope, crushing terrain and developed underground karst as well more potential hazard. All of which have led to scattered space planning of the city, urban land supply shortage and poor in quality, difficulty in road and greenbelt construction. But poor condition of land-use and scattered layout brings high economic costs to urbanization, which brings negative impact on the development and construction of Guiyang city. Therefore, in urban development in the future, we should choose intensive and efficient use of land resources to make compact urban structure and prioritize public transportation to ease the tension of urban construction land use and reduce economic costs in urbanization. Furthermore, it should also pay attention to strengthen landscape management and space control in Guiyang in order to achieve the coordinated development of urban and landscape.
Analysis on the factors effecting tourists' perceptual image in calligraphic landscape scenic-A case study in Diecaishan, Guilin
KE Li, ZHANG Jie, LI Qian
2010, 29(1): 87-92. doi: 10.3969/j.issn.1001-4810.2010.01.015
Abstract:
Diecaishan, a scenic concentrated with inscriptions on precipices in Guilin, is chosen as the example in this case study. The tourist’s perception to calligraphic landscape is extracted through influence factor analysis and the differences in perceptual image are researched in light of demographics of the tourists. It is found that the tourist gender has obvious difference in perception to factor “practice and interest”, female is more liable to be infected environment and has stronger perception to practicing interest than male; the perception to factor “association and brain development” is remarkably effected by the educational level received, Good-educated tourist has higher perception to the calligraphic landscape appreciation. Perception differences of different-motivated tourists to calligraphic landscape in Diecaishan are contrasted by means of one-way analysis of variance. It is proved that there are obvious differences in perception to factor “practice and interest” and factor “geographic mark” in different-motivated tourists.
Eco-tourism image positioning for Dashiwei Tiankeng group on the basis of comprehensive fuzzy evaluation
BAI Jin, ZHOU You-you, WANG Wei
2010, 29(1): 93-97. doi: 10.3969/j.issn.1001-4810.2010.01.016
Abstract:
Modern tourism brings about many image perceptions to tourists, which affect their decision to choose tourist site. Dashiwei Tiankeng has the tourism resources of world-class quality. But some factors like inconvenient traffic conditions and precipitous relief usually bring about prejudice to tourist’s sensation. The background image of Tiankeng scenic is expounded and the attractiveness of the Tiankeng resource is evaluated and analyzed via questionnaire surveys from experts and AHP evaluation in this paper. And after that, the factor’s attractiveness scores in each group of the Tiankeng scenic is computed by means of multilayered comprehensive fuzzy appraisal method. The results show that the Tiankeng traffic resource is of high attractiveness,the feature of landform, geology and animals and plants get 89.71 points, the scientific and visual value in resource 87.08 points, and curiosity of the Tiankeng gets 87.57 points. Hence, the advertisement for the Tiankeng traffic resource should be focus on rarity, completeness and typicality as well curiosity in geology, geomorphology and animals as well as plants.
Analysis on the influencing factors and disposing measures for cave accident relief
ZHOU Jun-liang, SONG Rui-ming
2010, 29(1): 99-101. doi: 10.3969/j.issn.1001-4810.2010.01.017
Abstract:
This paper summarize initially the influence of the factors, concerning cave temperature, humidity, surrounding, formation, structure and biology, upon cave accident assistance, by analyzing the caves environment of common types, and presents the necessary works for cave accident assistance, including basic equipment preparation, well-directed training, scene investigation, real-time command and backup support. Meanwhile, in view of the special for cave accident assistance and the function of fire-fight brigade determined by the revised Fire Service Law in this year, the paper propose the necessity and feasibility for built a government mountain emergency rescue system which is composed principally of fire-fight brigade and supplemented by the units having the ability of accident assistance and the nongovernmental relief for mountain emergency.
Legislative proposals for prevention and control of rocky desertification
MA Hong-chao
2010, 29(1): 103-105. doi: 10.3969/j.issn.1001-4810.2010.01.018
Abstract:
Among natural disasters which result in decrease of plantation and deterioration of land resource, except the well known desertification and salinization by us, there is another kind of disaster- rocky desertification of land, which is also called “The Earth Cancer” and erodes 2 500 square kilometers of land per year. Besides natural factors, over exploitation of land by human being is the main cause of rocky desertification of land. The basic reason for rocky desertification becomes a severer natural disaster than desertification is the shortage of institutions on planning of natural resources and statutes for controlling, resulting in ambiguity of rights and obligations on utilization of natural resources. The developing speed of rocky desertification is astonishing and the harm is serious. Meanwhile, the control of rocky desertification is also facing with a good chance. The 17th CPC National Congress proposed a strategic objective to build ecological civilization and definitely ask for enhancing governing rocky desertification and promoting ecological rehabilitation. China has raised the prevention and control of rocky desertification to an unprecedented level. Solution of problems in the process of control relies on laws and regulations to make clear rights and obligations of relative persons. However, laws and regulations on control of rocky desertification are almost blank. Thus, the author demonstrates feasibility of legislating to control rocky desertification in this paper and starts to explore and study legal countermeasures in the hope of making contribution to control rocky desertification.