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  • 1999 Volume 19 Issue 3
    Published: 20 May 1999
      

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  • Zheng Du, Fu Xiaofeng
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    Regional study is an ancient and important tradition, forming the regional school of geography. In view of integrated or unified geography, regional study of sustainable development is an important level for approaching regional system of man-land relationship and effective way for coordinating man-nature relationship. Aimed at sustainable development the integrated geographical regionalization includes natural elements and human factors. Main principles for demarcation are as follows: combining regional differentiation of physical environments and human geography, integrating comprehensive analysis and principal factors, genetic unity, as well as linking regional frameworks with regional types, etc. Criterion and index system of the integrated geographical regionalization consists of environments, resources, economy, society and population, etc. The selected criteria and indices for demarcation should be practical, simplified, comparable, quantified, and reflecting dynamic state and trends of various regions. Regional types of development states may be identified based on the above mentioned results, then proposing a tentative scheme of the integrated geographical regionalization.
  • Cai Yunlong, Meng Jijun
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    Land degradation is a major representation of global environmental change. In degraded land, people get into the trouble of PPE (poverty-population-environment) spiral. Land degradation takes various forms in China, such as land desertification, soil erosion, farmland pollution, surface mining, farmland salinization and soil fertility deterioration. Among these the former two are the most distributing and the most influencing. A great amount of poor population assembles in these lands, for example, in the karst areas of southwest China and in the Loess Plateau of northwest China. This paper especially pays more attention to the reversal of impoverishment-degradation spiral in the karst areas of southwest China. Since the PPE spiral is caused by ecological and, in particular, social factors, the solution must be in a social approach. Poverty alleviation is a systematic project with great complexities. Any single approach can not success and integrated measures should be taken. Obviously, the key to escape the vicious spiral is the reconstruction of the local ecosystem, economy and society so that the self development capacity of the local people may be enhanced. Thus the poverty can be essentially eliminated. On the other hand, it is unrealistic to let the degraded land naturally recover under the pressure of population growth and economic development. The degraded land needs ecological reconstruction through social investment, while the local economy and society should be restructured. Ecological reconstruction of the degraded land involves not only the degraded and underdeveloped localities but also developed regions. The guidelines of degraded land reconstruction should be the concepts of sustainability and economic viability, and the theory of landscape ecology. Sustainability includes the idea of a type of development that does not compromise, and even promote, the future use of land. Economic viability is profitability of the reconstructed land, although in a long term consideration. In other words, the reconstructed land and its use should obtain productivity, stability, sustainability, equability and autonomy. According to landscape ecology, reasonable land use and landscape patterns should be allocated at a macro scale, and an appropriate productivity and ecological conditions should be created at a micro scale. It is necessary, in the degraded land reconstruction, to identify different issues at different spatial scales, for example, land productivity at site, land use pattern at local, urban rural relation at a region, and economic cooperation at inter region. In temporal scale, it is necessary to establish realistic targets of short term (to emphasize viability), middle term (to get into benign spiral) and long term (to realize sustainability) respectively. As a social approach, the reconstruction of degraded land includes ideology innovation, institute transformation, and science and technology popularization.
  • Dang Anrong, Yan Shouyong, Wang Shixing
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    Using GIS as an analyzing tool, the characteristics, reasons, and trends of spatial variation of China’s grain yield are studied quantitatively based on the national grain production database ( by county unit ) in two periods (in 1985 and 1994). The result is that the increase of China’s grain yield in the past decade was very obvious, especially in north area, while the decrease of grain yield was exist in some of the south area of China. The increase of grain yield in north area was mainly come from the improvement of grain production condition while the decrease of grain yield in south area was driven by the comparison profits.
  • Li Bingcheng
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    The processes of desertification in dry regions have occurred mainly in the lower reaches of rivers. The channels of the processes of desertification have principally 4 sorts: producing sands on the spot, wind erosion on oases, drift sand intruding and flooded gravel burying oases. The substance of the processes of desertification is a sort of process of the oases transference that had happened owing to the moving and redistribution of resources of water of oases by virtue of mankind’s un-reasonable action of land exploitation. Along with the processes of transference, original oases had shrurk and new oases had emerged. The desertification had occurred in one place, and new oases had been formed probably in other areas. The oases are principally the outcome of resources of water. So long as there are not great changes in atmospheric circulation and total amount of water in the valley, the general area of the oases will not alter greatly in the valley. Desertified land can reverse under definite circumstances, but the reverse in dry regions is nearly impossible.
  • Zhang Feng, Zhang Longsheng, Shangguan Tieliang
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    There are various types of wetlands of 2145 km2 in Shanxi, they are distributed on the river valleys, lakes and reservoirs, and around lakes and reservoirs. The wetlands in Shanxi are rich in biodiversity, including 455 species of animal and 1209 species of plant, and there are 70 plant communities. Moreover, the situation and cause that biodiversity is under the threat is detailed analyzed, and the strategies for biodiversitys protection are discussed in this paper.
  • Deng Huiping, Liu Houfeng, Zhu Tingcheng
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    In this paper, temperature changes and precipitation fluctuations over Songnen Steppe since are analyzed 1953. Based on a soil water balance model and a climate yield empirical model, the impacts of recent forty years and future changes of temperature and precipitation on soil water and grassland productivity are estimated. Over forty years, winter and spring temperature have increased by 2.0℃ or so; autumn and annual temperature have increased about 1.0℃; summer temperature increased by 0.2℃. There is not a trend in precipitation changes. The impacts of temperature increase since 1953 on soil water and grass yield are small, the changes of soil water and grass yield are mainly dependent on precipitation changes. In CO2 doubling situation, according to GISS and GFDL GCMS outputs, temperature will increase by 3-6℃ and precipitation increase about 10% over Songnen Steppe. Such changes in temperature and precipitation will result in soil water decrease every month, while evapotranspiration will increase during rain season. Grass yield will decrease by 3%-4%.
  • Wang Qing
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    To the same Holocene relative sea level (base level) changes along the Northeastern Shandong peninsula, different rivers have adopted two different geomorphic response ways. In the middle and lower Dagujia type river valleys, there are backfilling and headward erosion stages which accompanied relative sea level rising and falling stages respectively, and there are still differences among rivers with different scales. In the Huangshui type river valleys, no aggrading and incising stages, which resulted from the Holocene base level changes, have been found, and the valleys have only played a role of transporting the debris from the upper drainage basins into the sea. For the middle and lower Dagujia type rivers, the meandering and braided river systems have developed in response to the relative sea level falling and rising respectively.
  • Li Tuansheng, Xiao Duning
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    Scale analysis is increasingly paid attention to in landscape ecology. This paper divideds Shenyang City into 12 landscape divisions with landscape scale analysis. Through landscape division, we find that landscape divisions of Shenyang City distribute irrationally, the same type of landscape divisions scatters and industrial landscape divisions are racher more.
  • Gu Chaolin, Liu Haiyong
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    Marxism geography had been a very important school of western human geography, although the socialism system in the Soviet Union and Eastern Europe was terminated it tended to be on the wane. Western Marxism geography emerged in the early 1970s in response to two sets of events: (1) The critique of "establishment geography", i.e. positivist, spatial analysis, behavior geography, and so on; and (2) the political uprisings of the late 1960s. David Harvey played a key role in the rise of Marxism geography, and his highly influential "Social justice and the city" was regarded as the consummation of Marxism geography. Marxism geographical research and writing can be treated under three headings: (1) political economics, which uses political economic analyses to explain the geography of capitalism as the outcome of political and economic relationships and progresses in the wider society; (2) theories of space, which highlight the reconstruction the relative conception of space; and (3) theories of nature and environment, which point the fundamental interconnectedness of society and nature. The first developing phase of Marxism geography lasted until the early 1980s, from which the new phase began. The new phase has brought not only the internal maturity but also the increasing challenges from outside, such as the critique of Humanism, Realism, Postmodernism and Feminism. Facing more and more challenges and debates, new Marxism geography took its rise from theoretical needs and the current political and economic situations. Since the socialist system demolished the capitalism and minimized the scope of class contradictions, in China, the academic field of geography lacked the background of class conflicts between working class and capitalist, which is the prerequisite of Marxism theories. As far as the integrity and maturity is concerned, the Western Marxism geography should be treated as an important source of reference.
  • Dai Junhu, Cui Haiting
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    Being a main section of land ecosystem, mountain regions are also synthetical systems of human and nature, which occupy one third of total land area, and can affect lives of half of the world population. As a result of the economic development of mountain regions recently, a lot of places are deteriorated. One muse attention to such areas. As a special region between closed forest and alpine meadow, alpine timberline always plays an important role in mountain ecosystems by being an incentive directive body to changes in such regions. But there were far less studies on alpine regions than on any other kind of ecosystem in the past, especially in China, let alone to find studies on alpine timberline and the relationship between alpine timberline and global climatic change. In order to do further studies on the ecotone between forest and alpine meadow, it is important to know what were done in the past and what is being doing now about it. The main purpose of this paper is to give a review in such a field. Based on the definition given by the former studies, a synthetic understanding is put forward by directing the main features of alpine timberline. It is an ecological ecotone; and the border of closed forest should consist of trees which have symmetric canopy and higher than 2 meters; the appearance of the ecotone is marked by so called krummholz; and the shrubs are not included in this belt. The characteristics of the studies on alpine timberline are forwarded by dividing it into three periods. In a word, the studies focus on different contents during each study period. As in the first period, it was very popular for the authors to describe this ecotone, such as the appearance of the ecotone, the main components of alpine timberline, etc; then the relationship between the alpine timberline and the environment was discussed; during the last period, the studies on alpine timberline are related to global climatic change. The main contents and methods of such studies are discussed inside the paper, including main methods of obtaining proxy data. The studies of alpine regions by Chinese scientists are also put forward. As a result, it is regarded that the importance of such studies is of great value. At last, several schemes of the studies in the field of alpine timberline in China are listed for the first time.
  • Liu Zhaoli
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    Rapid development of computer technology brings about emergency of interactive interpretation of remote sensing images on computer screen. It holds higher precision and can directly enter geographical information system. More attention should be paid to its low efficiency. This paper shows the method of vector trace of distinct objects in screen digitalization of remote sensing images. With equal and higher precision, the method can greatly enhance the work efficiency, and possesses the important significance to the design and development of special software for manual screen digitalization of remote sensing images.
  • Li Xiubin
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    Abstract There is an increasing concern about spatial equality of development as a social issue in China. Controversial arguments exist about the seriousness of the issue, mainly because of the difference among measuring methods adopted by different researchers. As a matter of fact, “a simple and intuitively satisfactory measure of equality” still remains an issue of speculation. In this study, the author took a spatial visulization approach instead of a numeric indicator to describe the spatial inequality of development in China. A statistic in geostatistics, spatial mean, was used as a means of spatial equality measurement. Values of the spatial mean for population, GDP and consumption level were plotted on the country map with the help from a Geographic Information System (GIS) of provincial level data of China. Location of the spatial mean for population was adopted as a reference point. If the spatial mean of the data (GDP and consumption level) is significantly different from the reference point, it indicates the spatial inequality of development. Distance of the deviation indicates the magnitude of inequality, while the direction of the deviation indicates the high density part of the country in terms of the concerned economic indicator. Results of the case study were compared to that of the work conducted by the Development Research Center of State Council of China, which adopted a modified version of standard deviation by employing Pearson’s coefficient of variation. Conclusions of the two studies are quite close to each other, while the visulization approach provides more information like the spatial form of the development inequality.
  • Zhang Erxun
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    On the base of GIS, by using the land grading and appraising information system, fist determine the factor, balance of land grading of Guanxian City proper, Shandong province, calculate the point value of all factors and units of land grading then according to the point value of unit, give the land grading a tentative dividing and field calibration, study the achievements in land grading.
  • Yang Zisheng
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    The value of R, erosive force of rainfall,is one of the basic factors used for setting up soil loss equation.Through analysing the data of soil erosion and erosive rainfall measured on the standard runoff pot,the best index in the northeast mountain region of Yunnan Province for calculating the erosive force of rainfall is defined as: R=E60·I30. According to this index and the data of rainfall from 16 stations in 1980-1997,we calculate the erosive force of rainffall (R) of every station in the northeast mountain region of Yunnan Province, and analyse the time space distribution characteristics of erosive force of rainfall in this region.The results of the calculation and the analysis show that the average annual value of R in this region is 293.8J/m2.For the distribution in a year,the value of R is higher in June~August,equivalent to 77.68% of the annual value.The annual variation of the value of R is also very large with a maximum of R 726.5J/m2 in a year to a minimum of R 94.2J/m2 in a year. For the spatial distribution,the value of R in northern area was higher than that in southern area,and in the dry and hot valley of the Jinsha River is lower than that in high altitude mountain zone.
  • Wang Jiading, Zhang Zhuoyuan, Li Baoxiong
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    The principle of earth microtremors is briefly introduced and the processes of saturated loess liguefaction induced by earth microtremors are analyzed from a dynamic view. A field test of loess in water immersion was done over a 420-hour period on the Gaolan Mountain in Lanzhou, China. After stopping water flooding, earth microtremors at the bottom of test impounding pits were continuously measured by seismic equipment. We conclude that there is a relationship between loess collapse values and the amplitude and predominant period of the earth microtremors. The results show that the higher the amplitude and the longer the predominant period of earth microtremors, the more intensive the liquefaction grade will be. Finally, the most probable series of affecting factors to liquefaction, such as C, φ values of loess, amplitude, frequency, duration and wave type of microtremors are all favorable to loess liquefaction.
  • You Kunyuan, Zhu Dakui, Shi Xiaodong
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    The tidal saltmarsh is the most marginal part of the marginal marineenvironments and the exact limit between marine and continent. Saltmarst has some sedimentary environmental Characteristics: the obvious vertical zonation of various environmental factors; greatvariations of every environmental parameter, compared with typical marine or terrene environment; a slight slope, on which the environmental succession from marine to continent is clearly divided and the vertical environmental succession in sediments is greatly amplified in lateral plane and so on. Tidal saltmarsh environment controls the features and distribution of saltmarsh foraminifera. According to the study abroad, the vetical zonation of saltmarsh foraminifera can be used as indicators for relocating former sea levels to an accuracy of ?20cm, even ?5cm. This quite high accuracy is important for studying sea level change, environment evolution and global change.
  • Huang Zhenguo, Zhang Weiqiang, Cheng Tegu
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    The tidal stations in Hong Kong and Macau provide the longest tidal records since 1925 along the coastal region of the South China Sea. However some abnormal errors or omissions during 1953-1956 and 1930-1949 in Hong Kong and 1963-1981 in Macau can be seen. Therefore taking 1959 as a connexion to continue the previous stage of 1925-1958 in Macau with the latter stage of 1959-1996 in Hong Kong, an impartial monthly mean series of sea level starting unify from the sea map base level of Hong Kong during recent 72 years (1925-1996) can be obtained. The sea level curve reveals a fluctuation tendency of sea level rise including abnormal higher and lower sea level, the former is related with the runoff of the Zhujiang River and the latter is in keeping with the strong El Nino year. The rate of sea level rise is calculated as 1.8 mm/a in recent 72 years using by single linear regression, and 2.0 mm/a during 1959-1994 dispeling the high frequency components from Fourier Transform. In addition dividing the series into 11 sets of 1955-1994, 1956-1994...1965-1994, and then calculated the average rate as 1.64?0.25 mm/a. Therefore the rate of 1.8?0.1 mm/a is epitomized from the tidal data in Hong Kong and Macau. The elevation of beach rock, earthquake activity and ground deformation indicate the relative stability of structure in Hong Kong and Macau, so that the rate of 1.8?0.1 mm/a can be deduced as the rise rate of theoretical sea level along the coastal region of South China Sea.
  • Huang Xichou, Huang Fang
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