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  • 2002 Volume 22 Issue 5
    Published: 20 September 2002
      

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  • LIU Xiao-dong, AN Zhi-sheng, FANG Jian-gang, CHEN Guang-shan
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    Using the recent 50-year precipitation data observed at weather stations and nearly-400-year precipitation data reconstructed with historical documents and tree rings in the Yellow River valley, the relationship between variations of the precipitation and global average temperature was examined by regression and composite analyses. The results show that the higher (lower) global average temperature corresponds to the less(more)-than-normal precipitation in the middle reaches of the Yellow River to a certain degree on different time scales. When the global mean air temperature increases by 1℃, the annual precipitation is found to decrease more than 20% over the middle reaches of the Yellow River from Shaanxi to Shanxi provinces. The difference between the annual precipitation averaged for the warmest three years and that for the coldest three years can reach 40% in the study area in last 50 years. However, the annual precipitation near the area of China-Mongolia boundary is decreased with the global warming. Our result from the observational study is consistent with that obtained from climate models under conditions of the atmospheric CO2 doubling and the global climate warming. The present result also shows that August-September, late summer-early autumn, is a key period which determines inter-annual variations of annual precipitation in the middle reaches of the Yellow River. The variation of August-September precipitation contributes more than 50% variance of inter-annual variability of annual precipitation in this area. Moreover, it is found that there is a close relationship between the rainfall anomaly and activity of the subtropical West Pacific High in August and September. A warmer global climate may intensify and enlarge the subtropical West Pacific High, thus induce the front of East Asian summer monsoon to move northwards and to act frequently there, and eventually bring about the decreased rainfall in the south side of north boundary of the East Asian summer monsoon. The situation will be opposite when the global climate becomes colder. This study suggests that we should pay great attention to the dryness induced by the global warming over the Yellow River valley.
  • PAN Bao-tian, GAO Hong-shan, LI Ji-jun
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    Planation surface is a remnant of landform in old age and the erosion surface is of a mature landform, according to the Davisian cycle. Studies on the long-term landscape evolution show that there are four types of planation surface, peneplain, pediplain, double leveling surfaces and cryoplain. The peneplain is formed through lowering of relief in wet region. The pediplain is developed by slope retreating in dry region. The double leveling surfaces appeares in Savanna landscape. The cryoplain is formed in periglacial environment. Measurement of erosion rates and retreating rates of slope indicated that formation of planation surface needs the tectonic equability for severl million years or thousands million years. In the the Qinghai-Xizang Plateau, there are two planation surfaces and one erosion surface, Summit Surface, Main Surface and Erosion Surface. The Summit Surface have formed in the Oligocene and early Miocene, and the Main Surface between 20-3.6Ma B.P. Tectonics on the Qinghai-Xizang Plateau were relatively stable between 3.6Ma B.P. and 1.7Ma B.P. and the Erosion Surfaces was formed. Because the Main Surface is a "jumping-off point" of the Qinghai-Xizang Plateau, studies on its mode of formation and height have great significance in determining the altitude of the Qinghai-Xizang Plateau before uplift. Synthesizing the proofs from mammal fauna, regolith and geomorphology, we think the Main Surface was developed as a typical double level surface. There could be the peneplain in the south of it and the pediplain on north. Its altitude should not exceed 1000 m when it was formed. The Intense tectonic uplift, which resulted in the present Qinghai-Xizang Plateau with an altitude of 4500-5000m, happened in last 3.6Ma when the Main Surface was destroyed.
  • WANG Gen-xu, WANG Jian, WU Yan-qing
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    Selecting the 13 items of land use or land cover index, which indict the changes of regional eco-environment, from the remote sensing data of 2000 over the whole river basin with an area of 13.0?104km2. At the same time, the remote sensing data from 1987 was analyzed to output the eco-environmental index of 1987. Comparing with the two time phase analysis results of eco-environmental index, and integrating the field surveying results, the trends and extent of eco-environmental changes in the Heihe River basin were analyzed. The features of eco-environmental changes were quantitatively discussed. Those features showed that, in recent 10 years, the eco-environment of the Heihe River basin was degrading as a whole. Forest area in the river basin decreased by 6.35%. The middle reaches, which replaced the lower reach, was the most serious desertification region, and the upper reaches was the rapidly exacerbated desertification region. Grassland ecology showed a continuous degradation tendency in the lower reaches, the total area of degraded grassland occupied 2095.39km2. But in some regions of the river basin, the eco-environment was improved.
  • HU Jin-ming, CUI Hai-ting, LI Yi-yin
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    Using the field archaeological data and some research results in archaeology and environmental evolution, this paper analyzes the historic evolution of the cultural landscapes and natural landscape since the Holocene in the Xiliao River Basin. Based on the historic evolution of natural and cultural landscapes, the authors systematically reconstruct the coupling evolution history of man-land system and unveil the interactional mechanisms between human and nature in the Xiliao River Basin.During the earlier Holocene, evolution of pre-historic cultures, including Xiaohexi Culture and Xinglongwa Culture, had been closely linked with climatic evolution. Climatic changes into warm and humid resulted in the germination and development of the pre-historic cultures, while decline of pre-historic cultures had close relationship with climatic deterioration. During the middle period of the Holocene from Zhaobaogou Culture to Lower Layer Culture of Xiajiadian, prosperity and decline of cultures correlated with multifold factors. Evolution of natural landscape was the external driving force. While humańs cultural accumulation, inter-regional cultural diffusion and intercommunication were the internal driving forces. Humańs disturbances upon natural landscape would feed back to cultural landscapes and influence the development of cultures. Cultural transformation between Upper Layer Culture and Lower Layer Culture of Xiajiadian was a gradual changing process. Climatic change was the main driving force, while inter-regional cultural communication further advanced the development of animal husbandry of Upper Layer Culture of Xiajiadian.During historic period, multifold factors, such as prosperity and decline of the Han and minority dynasties, ethnic policy of the Han dynasties, cultural intercommunication between the Han nationality and minority, development of social productivity level, changes of natural environment, etc, comprehensively acted on the evolution of cultural landscapes. In fact, it was the ebb and flow of different nationś cultures, which were the most important. Development of culture and productivity level promoted humańs ability to adapt to and remodel nature, and culture played more and more important role in the evolution of man-land system.
  • REN Mei-e
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    The earliest courses of the lower Yellow River are: the Yugong River and Shanjing River. Near Zhengzhou, Henan Province, they both turned abruptly to the north along eastern foot of Taihang Mountains to north of Beijing. It is suggested that this may be due to a great earthquake of 4280 a B.P. in Taihang Mountains. There is also an E-W active fault in Yanshan Mountain with its downthrow side on the south. The Shanjng River probably followed this fault valley and entered the Bohai Sea north of Tianjin.
  • WANG Zhang-hua, CHEN Zhong-yuan, KOU Ying, CHEN Yu
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    The present study collected historic climatic records since 960 A.D. from the Taihu drainage basin. A dry/wet series, i.e. a five-grade index of severe flood (1), flood (2), normal (3), drought (4), and severe drought (5) from 960 A.D. to 1992 A.D. was reconstructed and χ2-test was used to examine the evenly distribution of the series. Power spectrum analysis was made for the present 1033-year dry/wet grade series with different lagging of 280, 200, and 150. Process of "Red Noise" was applied to make the significance test (α=0.05). Moving t-test was applied to detect the abrupt climate changes of the study area. The 11-year and 30-year moving average curves and their 6-degree polynomial regression curves are also presented to help the detection of climate jump. Spectral analysis reveals that the change of drought-wet climate in the study area was a superposed phenomenon with the major period of ~100-year, and other notable periods of 36-year, 26-27-year, 11-year, 22-year, 15-year, 19-year, 2-3-year, 8-year, and 5-6-year. Compared with those of celestial activity and climate change collected by previous work, these periods are supposed to be closely related to the celestial activities that control the planetary wind system and East Asia monsoon circulation. The moving t test detected two large-scale abrupt changes, i.e., 1247-1263 A.D. and 1618-1635 A.D. The climate between these two abrupt changes was relative humid. Before 1247 A.D. and after 1635 A.D. it was relative dry. The 14th to 15th centuries was the wettest episode during the last 1000 years in the study area. This getting-humid event occurred widely in East Asia.
  • LU Jin-fa, LIU Ai-xia
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    Thirty-six river basins, where the data of measured grain size of sediment are available, were chosen for an analysis on relationships between grain size of sediment and rainfall features in the middle reaches of the Yellow River. These basins fall into 5 types of different physio-geographical environments. Annual average rainfall, unevenness, seasonality and yearly variation of rainfall were taken as the indices of rainfall to relate to grain size of sediment. It was shown that good linear positive multi-relationships exist between grain size of sediment and seasonal and annual variation of rainfall when taking the different types of basin as perameters, but simple non-linear relationships between grain size of sediment and annual average rainfall and unevenness of rainfall. Vegetation, surface material and landform exert an important control on the relationships between grain size of sediment and rainfall features. Different slope and positions of curves were observed in the relationships between grain size of sediment and seasonal and annual variation of rainfall for different types of river basins. The slope of curve decreases and the position moves down subsequently from the basins of windy sand, sandy loess and heavily weathered siltstone and mudstone to those of loess and clayey loess. The different positions were also observed in the relationships between grain size of sediment and annual average rainfall and unevenness of rainfall for different types of river basins. From the upper to the lower of the curve the type of river basin changes from the basins covered by windy sand, sandy loess or heavily weathered siltstone and mudstone to those of loess and clayey loess subsequently.
  • WANG Hong-ya, WANG Mei-hua, XIE Qiang, YU Peng-tao, LIU Hong-yan, CUI Hai-ting
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    AMS 14C dating, analyses of grain-size, CaCO3 content, δ18O and δ13C in carbonates, content of organic matter, TOC content and C/N ratio, and measurements of χlf and SIRM are performed with sediments, consisting mainly of peat, from a profile near Huashaoying Town (114°36’E, 40°18’N), the eastern part of Nihewan Basin. The results indicate that these sediments were deposited mainly during 5320-3370 a B.P.; the climate was still rather humid and warm during 5320-3600 a B.P.; there was a marked dry/cold-and-dry event occurring respectively at 3600-3460 a B.P. and 3430-3400 a B.P. Such climatic fluctuations might be the terminating process of the mid-Holocene wet conditions.
  • WANG Shi-jun, CHEN Cai
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    This paper reviews and summaries the four stages of economic geography development, and the features and contributions in each period in the last 50 years, emphasizing on the recent two decades. And also, it analyzes the framework of current Chinese economic geographic theory, and points out that this subject consists of one core, two directions, dual characters, three fields, three basic theories-industrial structure network theory, regional division of work theory and economic region movement theory, and such branch theories as condition theory, industrial factors theory, structure and function theory, and geo-relation theory. The three basic theories are the supporting skeleton of this subject, being relative stable, while the branch theories vary according to the elasticity of its study substance, being relative unstable, owning clear time characters. Finally, this paper points out four trends of economic geographic theory development, namely, "centrifuge" and "return" of the subject, resuscitation of industrial economic geography, the strengthening of the research on geopolitical and geoeconomic theory, and hot spot of regional development and regional image design.
  • NIAN Fu-hua, YAO Shi-mou, CHEN Zhen-guang
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    Under the new circumstances of global economic integration, industrialization and the urbanization promote the rapid development of IT industry, especially ’information expressway and internet’-based on computer and remote-sensing technology among big cities gets faster development. Information network has great influences on the formation and the development of urban agglomeration. The network of urban agglomeration is not only the most superior model in material flow between cities and countries, but also is the optimized urbanization model on the process of formation of urban agglomeration. The network organization of urban agglomeration is being perfected and has all kinds of models in the area of well-equipped infrastructure. The article focally discusses the following issues: ①The conception and the spatial distribution of network in urban agglomeration. ②The four network models of urban agglomeration: core region network, towns of dumbbell network, multiple nuclei network, corridor-type network.③The influences of network on the flows of people, material and information in urban agglomeration. Based on the analysis on the reasonability of network in view of spatial organization, the authors try to adjust the contradiction between the planned economic activities and disorderly management.
  • LI Wen-ling, YAN Xiao-pei
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    Based on the recent development of MTR(Mass Transportation Railway) system in Guangzhou City, we analyzed the effects of the land compound use along the MTR lines, and studied the raised problems between the development of MTR system and the land compound use. With the construction of the metro transport in Guangzhou City, the developed axis of the city was shaped quickly, the function of the city center was strengthened, meanwhile the old city was transformed and the land replacement was speeded up, and the unanimous of the land type was urged. However, it also supplies an opportunity to develop the underground space of the city, and has been making an enormous influence on the land revalue along the metro transport lines. As the development of the metro transport in Guangzhou was being starting stage, it is necessary to take nice syntheses plan and design on the MTR lines selection, management, and development of land along the lines.
  • CHEN Yan-guang, LIU Ji-sheng, FANG Yan-gang
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    Many basic mathematical models as scale laws can be derived from a pair of assumptions, i.e. ① The utility in some sense is proportional to some kinds of variables such as time, space, and class; ② The respondent variables of the utility such as population size and city number is the exponential function of the utility. The basic models include the allometric relationship of urban and rural population, logistical model of urbanization process, the relationship between level of urbanization and that of economic development, i.e. Zhou’s model, urban population density model, i.e. Clark’s model, the generalized Beckmann-Davis model, and the three-parameter Zipf model, etc. It is proved that the exponential relationships between the utility and its respondency come from utility-maximization that is consistent with entropy-maximization, and utility-maximization and entropy-maximization are actually principles of duality. Ont the other hand, the basic models for analytical urban geography can be changed into logit models, for example, the urban and rural population allometric model is linked to binary logit model (BLM), and the Clark model can be connected with multinomial logit model (MNL). This means that we can simulate the urban dynamics based on utility-maximization principle by means of logit transformation that can simplify the researched objects to a great extent. The logit transformation will become an important part of geocomputation and the simulation based on the logit models consociated with utility-maximization principle will contribute to the studies of spatial complexity. Utility-maximization is not only one of the general principles of urban geography but the foundation of urban maximization from which we can develop new methods for urban planning. Perhaps the consistence of utility-maximization and entropy-maximization is the key to solving the problems of spatial complexity. Unlike the concepts such as "the edge of chaos" and "self-organized criticality", the duality of utility-and entropy-maximization can answer many theoretical questions without using one concept to replace another.
  • XU Xiao-bin, WANG Jian, Françoise Yiou, Grant Raisbeck
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    Because of cosmogenic isotopes production, the concentration of cosmogenic isotope in surface layer of the exposed rocks accumulates more and more, and at same time, it becomes less and less with isotope’s radiation and surface’s erosion. With this principle, under the condition of cosmogenic isotopes production rate being well known, the function between the concentrations of cosmogenic isotopes and time and erosion can be calculated. Using this model, we can calculate the exposed ages and erosion rate of the surface. This makes the dating technique be very useful and have a good provision in the study of Geomorphology and Quaternary. In cosmogenic isotopes, 26Al and 10Be deriving from quartz are used most widely and maturely in this field.
  • DUAN Xue-jun
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    The Virtual Reality is a composite technique. It can create the lifelike feeling such as visual, hearing and smell sense, make people participate the virtual world, and give people the sense of being personally on the scene. The Virtual Reality System is composed of the hardware such as the graphic workstation, the display equipment and the sensor instruments; it is composite with 3D modeling, virtual scene driving and sensor controlling software, etc. 3D modeling, interacting, sensing and computing technique supports the Virtual Realty. The Virtual Geographical Environment (VGE) comes out of the using of the Virtual Reality in Geography. VGE makes it realized that the geographer could design and modify the geographical correlation, analytic and engineer model according to the personal technology, supposition and plan, and observe the result through interacting with it. With the developing of application of the Virtual Reality in Geography, the science of Geography will be explored more deeply. In geographical education, because the Virtual Reality expresses the technology and concept in lifelike feeling, the educated person will be more interested in it, and it may lead to better results. In theory study, the Virtual Reality may realize the virtually reappearing of the most part of geographical studying activity, which can help the geographer immerse in certain 3D scene wholly, so that they can give full play to their geographical ability of thinking and imagination. The virtual geographical experiments can be done by the Virtual Reality, which makes geographical simulation repeatable. Furthermore, the Virtual Reality is important in the practice of urban planing, tourism, and disaster prevention, and so on.
  • FAN Yue-jiao
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    This paper is based on an achievement of knowledge innovation project of CAS named the space-temporal information analysis of territorial environment by Remote Sensing and pre-research of relative theory and technique of digital earth (part of Southwest China). With the support of core database of the landuse types change, taking Three Gorges’ Project Area as investigated region, the characteristics of landuse degree changes were studied and analyzed deeply from 1986 to 2000 by using the integrative techniques of Remote Sensing and GIS. The core purpose of the article is to provide the theoretic basis and scientific methods of rational development, utilization and management of land resources for the local government and administration section. At the same time, it also provided methods for reference in the space-temporal variation of landuse in mountainous area.
  • FU Su-hua, LIU Bao-yuan, WU Jing-dong, DUAN Shu-huai
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    Runoff causes soil erosion and environmental pollution. It is very important for soil loss calculation and soil and water resources evaluation to select suitable runoff calculation method. The 30 single storm data of two conventional tillage plots at Puwa watershed, Fangshan County and 13 single storm data of one fallow plot at Shixia watershed, Miyun County were used. Several runoff calculation methods, including GAML revised by Chu, Phillip, Horton, SCS curve number, were compared. The results showed that the model efficiencies of GAML and Phillip were higher than those of Horton and SCS curve number. According to the parameters easily obtained, GAML revised by Chu is suggested when there are the continuous records of rainfall in Beijing mountainous area. If not, SCS curve number should be used. The results can be served as soil and water evaluation and plan.
  • SONG Chang-chun, DENG Wei, LI Qu-sheng, WANG Zhi-chun, ZHANG Guang-xin
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    The controlling of secondary soil salinization may take into account four main complex factors: leaching, groundwater table, time and modifier in the west of Songnen Plain. The change of salinity characteristic is analysed for soil profile during comprehensive harnessing and its effects on the characteristic of circumjacent soil are also studied. And through experiment, the paper studies the effects of different water-applying regimes on the changes of soil salinity in plowed layer. Based on a series of comprehensive experiments of applying soil amendment, the comprehensive technology system for preventation and treatment of soil secondary salinization in this region is established.
  • DONG De-ming, ZHAO Wen-jin, WANG Xian-en, FANG Chun-sheng
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    In this article, the shortages of traditional EIA are analyzed, the progress on the research and practice of SEA is reviewed, the relationship between SEA and environmental sustainable development is elaborated and the problems in the system of SEA, which aim to achieve environmental sustainable development, are analyzed.
  • DING Wei-xin, CAI Zu-cong
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    The paper reviews the abilities of methane production, oxidization and flux of different mire types and their influencing factors. The depth of water table affects the pattern of vegetation in mires, which, in turn, strongly influences the development and soil profile of mires, resulting in discrepancy in flux of methane emission from various mires. The patterns of methane emission in different type of mires and different season are as following: marsh > fen > swamp > bog, and summer > spring or/and fall > winter, respectively. The main factors influencing flux of methane emission from mires are the depth of water table, substrate, type and density of plant in mires, temperature, pH, exogenous nitrogen and soil basic properties.
  • WU Quan-yuan, MENG Fan-hai
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    Water resource optimization dispatch is very complex. The difference in space and time between water supply source and needs of economic departments for water, the translation relation between surface water and ground water and the compensate modulation between surface reservoir and ground reservoir should be considered. In principle of dispatch, the water supply’s allocation in different regions, departments, ways and corporations is confirmed, so as to make water resource benefit most. This article establishes the main restriction conditions, object function and principle of water allocation through detailed representation of the temporal and spatial relation of the Longkou water resource system. Based on these, subsystems of water resource optimization dispatch are established and experimental application studies have been done.
  • LI Xiu-jun, LI Qu-sheng, SUN Chang-zhan
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    Water-saving irrigation is important to develop agriculture and increase yields in the arid, semi-arid and semi-humid areas. An economical and effective irrigation management technique can save water and increase yields as well. This technique, based on a summation of researches both in China and abroad, takes moisture content, soil, plant and atmosphere as an integral part of the whole, sets up an water-balance equation by means of the law of conservation of matters energy. The equation is: Wsoil=Frainfall+Qirrigation+Worigination-Wrunoff-Wwither-Wpenetrate-nET cSuch physical parameters as soil unit weight, field capacity, withering parameter, original soil’s water content and etc. were surveyed. The meteorological data as temperature and rainfall from meteorological observation and forecast were obtained. The advanced method is applied to calculate crop’s transpiration. According to the relation between soil’s water content and crop’s transpiration, the irrigation time and amount are obtained. Thereby a proper irrigation system is determined. The application shows that this technique has the very good function to increased corn yield and save water.
  • WANG Ai-hua, ZHANG Shu-qing, HE Yan-fen
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    Based on landscape ecology, remote sensing and Geographical Information System technologies, the dynamic change of mire in Sanjiang Plain is analyzed. The results show that mire is mainly distributed in the counties of Fujin, Tongjiang and Fuyuan, whose area accounts for 51.42% of the total area of mire in Sanjiang Plain. The area of mire decreased greatly from 1980 to 2000, especially from 1980 to 1996, it decreased to 51.33%. Since 1996 the decrease speed of mire’s area has become slow. The results also indicate that the fragmentation of mire landscape was evident in the last two decades in Sanjiang Plain. The number of patch has increased 46%, and the density of patch has increased two times. The fractal dimension of mire landscape in 1980,1996 and 2000 respectively is 1.3121,1.3839 and 1.3631. This means that the shape of mire landscape greatly transforms. The area change of mire in other counties except the counties of Baoqing, Tangyuan, and Tongjiang is greater than the whole region.