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  • 1990 Volume 10 Issue 2
    Published: 20 March 1990
      

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  • Lu Jinfu, Li Zhimin
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    The loess in Liaodong Peninsula is mainly distributed below 70 meters underground along the Bohai coastal areas,with the thickness of 10-15 metres. The loess in Liaodong Peninsula can be classified into pro-Lishi stage,Lishi stage and Malan stage.The period of pro-Lishi loess is from the Pliocene to the early Pleistocene.The loess of Lishi stage can be divided into the lower Lishi loess and the upper Lishi loess.And Malan loess stage is the later period of the Pleistocene. The silver sand content in the loess of Liaodong Peninsula is much more than the silt content.However,there is the tendency that silt content gradually increases from the lower part Io the upper part of both Lishi and Malan loess. The major minerals in the loess are light ones,such as quarts,feldspar,etc. The source of the loess substances in Liaodong Peninsula are different,some came from the inland of Shandong and Shaanxi provinces,some from the nearby sea areas,and some was brought by rivers from the low mountain and hill areas.
  • Yang Qinye, Zheng Du
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    The Hengduan Mountain region(HMR)is a transitional zone from the Qinghai-Xizang Plateau to the Yunnan-Guizhou Plateau and Sichuan Basin,with mountains and deep gorges running in parallel from north to south,The vertical zonation here is very conspicuous,and the agricultural development in various altitudinal zones is very different, Vertical zonation,agricultural distribution(including plantation,forestry and animal husbandty)are discussed in the paper,The complex regional differentiation is correlated with the geographical location,and absolute and relative altitudes, From southeastern and southwestern margins to the interior,with increasing altitude,in addition to the differences of the basal belt,there is a decrease in number of vertical zones and simplification of spectra,The regional differentiation of upper forests limits and the dry valleys are discussed, It is considered that HMR is a complex ecosystem,in which the vertical zonation is a natural base of vertical distribution of agriculture,The exploitation and utilization of natural resources should be paid attention to,After discussing present agricultural situation,it is pointed out thai diversified economy development should be emphasized and taken as a fundamental policy;the mountain agto-ecosystem with forests as main parts should be established;the existing farm land should be fully utilized so as to increase per unit yield;economic forests and fruit trees should be vigorously developed;contradiction between plantation and animal husbandry should be well coordinated;and plantation,forestry and animal husbandry should be well developed together,So far as this,special farming system in HMR could be established.
  • Jiang Zhongxin
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    With the methods of regression analysis and trend surface analysis,taking the low and high lines of dark conifer forest,premafrost low line and the snowline of the latest glaciation in China as examples,the paper expounds the zonality regularity of the distribution of physico-geographical zone in China. (1)Latitude zonality obeys the mathematical model of normal frequency distribution,being approximate to descending straight line within the latitude range of China.(2)Latitude zonality shows that the elevation of physico-geographical zone rises straight with the distance to east coast line, (3)The combination of the distribution of latitude and longitude zonalities appears a plane inclining from SSW to NNE.The decline rate of the elevation of physico-geographical zone with latitude,from south to north is 54-143 meters per degree,and the rise rate of the longitude from east to west is 0,22-0,48 meter per kilometer.The decline rate along plane dip from SSW to NNE is 0.65-1.35 meter per kilometer.(4)The second order trend surface of physicogeographical zone resembles a semiellipse-sphere inclining from the QinghaiXizang Plateau to northeast China,reflecting the effect of relief.(5)Physicogeographical zonation depends on the combination of hydrothermal conditions, Thus the factors influencing the zonality distribution regularity of physicogeographical zone of China are latitude zone,the distribution of oceans and land, and relief features.(6)The change rate of permofrost low line is the largest, showing the permafrost low line is most sensitive to hydrothermal conditions. The data of the snowline of the latest glaciation are dispersive,indicating that the data of cast China have more errors.
  • Zhang Xianqi, Li Guanghe
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    With the isothermal adsorption equation,dynamical model of adsorption,one dimension convection-dispersion-adsorption-disadsorption finite element model,the paper studies the contribution and migration of Pb(Ⅱ)in soil of vadose zone under the condition of infiltration of solution at the different time arid depth of soil.Reliability of calculating models is demonstrated through contrasting soil-chemical data analyzed before experiment with that after experiment,and contrasting calculation results with the field soft-chemical data,which determine the mode of migration and distribution of Pb(Ⅱ)in soil of vadose zone.
  • Chen Chun, Wang Yeqiao, Bo Liqun, Wan Enpu
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    The rate of computer processing digital map,in certain extent,depends on the efficiency of intersection calculation of map vectors.Usually,the efficiency of intersection calculation is seriously decreased while the amount of map data increased.The paper presents an algorithm of intersection calculation for vector structure map data.The algorithm extract the child arcs which contain intersections by scanning the data of whole map,and make pair for each intersecting child arcs,then calculate the coordinates of intersections. The intersection calculation programs by using this algorithm has been adopted into the Regional Information System of the Sanjiang Plain developed by the Department of Image Processing and GIS,Changchun Institute of Geography. It makes an important role for the vector data processing.The intersection processing of vector data supplys a necessary condition to arc edition and automatic formating of polygon topological information.It reduces the limited requirement for the input of vector data and makes easy to input data.The program has been improved through running and maintaining of more than one year.The application results have shown that the algorithm has a high efficiency and great application value on GIS.
  • Wang Jian
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    Temperature of every month on both the upper and lower bounds of subalpine dark conifer forests at various sites in China are estimated in terms of their distributions and temperature records,Based on these estimated data,the heat factor to influence and control the distribution and growth of sub-alpine dark conifer forests in China are discussed.It is found that the most important heat index to influence and control the distribution and growth of sub-alpine dark conifer forests is neither the mean temperaure in the warmest month,nor the maximum or minimum temperatures,but accumulated temperature of >0℃ monthly temperature or effective accumulated temperature of >5℃ monthly temperature. When accumulated temperature of >0℃ monthly temperature is more than 40℃, or effective accumulated temperature of >5℃ monthly temperature is over 50℃, sub-alpine dark conifer forests cannot grow well.When accumulated temperature of >0℃ monthly temperature is less than 30℃,or effective accumulated temperature of >5℃ monthly temperature is more than 60℃,sub-alpine dark conifer forests cannot grow at all.When effective accumulated temperature of >5℃ monthly temperature is between 15℃-45℃,sub-alpine dark conifer forests in China can grow well.The ecological significance of temperature in May and September,and in summer half year are discussed.
  • Han Shuti, Zhong Wei
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    On the basis of the trace element analysis of ZK0024 drill in Barkol Lake in the Holocene,in combination with the data on the sporo-pollen,micropaleontology and 14C dating,the palaeoclimate significance from the evolution law of trace elements in ZK0024 drill of Barkol Lake since the Holocene is discussed. The higher and lower values of trace element ratios are corresponds to the warm -dry and cold-humid periods respectively.The regular change of trace clements and their ratios from bottom to top reflects the change of cold-humid and warm -dry alternation of palaeoclimate.The new idea is proposed that the cold-humid period corresponds to the glacial age and the warm-dry period to the interglacial epoch.It is considered that the palaeoclimate evolution pattern belong to the monsoon climate region since the Late Pleistocene.
  • Zhang Wenkui
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    Behavioral geography has become one of the most important branches in human geography since the behavioral revolution during the 1970s.It mainly concerns some problems like behavioral space,geographical image,mental map, behavioral location and so on. Behavioral space refers to the activity space sensed in human mind,including natural regions and perceived space.To have the knowledge of human behavioral space and the composing elements can help people master themselves behaviour and expand their spatial activity more efficiently. Geographical image is a kind of mental impression of people ori natural environment.It involves distance,direction and stereo scene of nature as well. This image is the base that people recognize the natural environment and make behavioral decision.So it is very important for human behavioral decision to clarify its characteristics and function. Mental map is a kind of diagram formed through the reappcarance of personal geographical image on natural environment.Studying the forming elements and the pattern of the map is beneficial to the spatial decision of the optimum activities of human being. Behavioral location is the location theory formed based on the behavioral therories.It involves some professional terms such as non-economic man and sat isfication,etc.With behavioral matrix,it mainly deals with the relationship between the location choice of human activities and the information utilization,to help people select the superior location of their activities.
  • Wang Shuhai, Wang Renhua, Liu Yang, Liu Jingshuang, Song Deren, Wang Zeping, Huang Guoqing, Du Zhenhua
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    Paddy field of 4000mu was polluted by waste water containing mylthmercury in Qingzhen District of Guizhou Province.The mylthmereury pollution index of paddy field was up to 60,thai of rice 7.The mylthmercury pollution index of well water in the district was up to 200,that of Hongfen Lake 50. Although the waste water containing mercury was treated,trace mylthmercury was still drained into environment,which was obviously polluted. The hair and blood in about 30% of people in the district accumulated mylthmercury,which came from rice and meat of domestic animals,but the content was lower than that of the people who eated polluted fish and shellfish. Otherwise,the district is located in NNE lava mountainous region,the stratum is dominated by carbonate rock of shallow-sea facies.Therefore it is possible that groundwater is polluted through permeation effect.
  • Feng Lihua
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    The Qiantang River basin is located in the monsoon climate zone along cast and south coasts,with abundant water vapour and plentiful rainfall.Within the basin,precipitation obviously corresponds to runoff,and runoff coefficient is stable.There are 11-year and 14-year quasi-cycle changes of natural runoff. There are three types of rainstorm and flood:typhoon,plum rain,thunder rainstorm.The river contains less silt,belonging to the clear water river with much more water and less sand.The Qiantang River is rich in water energy resources.Its mouth is a strong tide one.Tide energy is striking.The drop of the upper reaches is greal,so water energy resources are abundant.With the increase of industrial,agricultural and domestic water,to research deeply the hydrological law of the Qiantang River is very benefitial to utilizing rationally water resources and water energy resources,and promoting the economic development of the basin.