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Title of Journal: J Mt Sci

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Abbravation: Journal of Mountain Science

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Science Press

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DOI

10.1007/s11464-015-0433-7

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1993-0321

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Relief degree of land surface and population distr

Authors: Ying Liu Wei Deng Xueqian Song
Publish Date: 2015/03/24
Volume: 12, Issue: 2, Pages: 518-532
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Abstract

Evaluation on the population pressure in the mountainous areas is a necessary condition for the protection and good governance The evaluation depends on accurate population density assessment Traditional methods used to calculate population density often adopt the administrative region as a scale for statistical analysis These methods did not consider the effects of the relief degree of land surface RDLS on the population distribution Therefore they cannot accurately reflect the degree of population aggregation especially in mountainous areas To explore this issue further we took the mountainous areas of China as the research area China has A total area of 666 km2 can be classified as mountainous area accounting for 694 of the country’s total landmass The data used in this research included the digital elevation model DEM of China at a scale of 11000000 National population density raster data the DEM and the national population density raster data First we determined the relief degree of land surface RDLS Next we conducted a correlation analysis between the population distribution and the RDLS using the Statistical Package for Social Science SPSS Based on the correlation analysis results and population distribution this new method was used to revise the provincial population density of the mountainous areas The revised results were used to determine the population pressure of different mountainous areas Overall the following results were obtained 1 The RDLS was low in most mountainous areas with a value between 0 and 35 and exhibited a spatial pattern that followed the physiognomy of China 2 The relationship between the RDLS and population density were logarithmic with an R2 value up to 0798 p005 and the correlation decreased from east to west 3 The difference between the revised population density RPD and the traditional population density PD was larger in the southeastern region of China than in the northwestern region 4 In addition compared with traditional results the revised result indicated that the population pressure was larger Based on these results the following conclusions were made 1 the revised method for estimating population density that incorporates the RDLS is reasonable and practical 2 the potential population pressure in the southeastern mountainous areas is substantial 3 the characteristics of the terrain in the high mountainous areas are important for the scattered distribution of the population and 4 the population distribution of mountainous areas in China should be guided by local conditions such as social economic and topographic conditions


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Other Papers In This Journal:

  1. Influence of collective boulder array on the surrounding time-averaged and turbulent flow fields
  2. Impact of earthquake-induced landslide on the habitat suitability of giant panda in Wolong, China
  3. The optimal cross-section design of the “Trapezoid-V” shaped drainage canal of viscous debris flow
  4. Transpiration rates of Carex Meyeriana in relation to micrometerological factors in a mountain valley wetland
  5. Hybrid denoising-jittering data processing approach to enhance sediment load prediction of muddy rivers
  6. An empirical formula for suspended sediment delivery ratio of main river after confluence of debris flow
  7. Initiation and development of water film by seepage
  8. Determinants of household food security in Nepal: A binary logistic regression analysis
  9. Causes for the unimodal pattern of leaf carbon isotope composition in Abies faxoniana trees growing in a natural forest along an altitudinal gradient
  10. Monitoring glacier and supra-glacier lakes from space in Mt. Qomolangma region of the Himalayas on the Tibetan Plateau in China
  11. Uncertainty of slope length derived from digital elevation models of the Loess Plateau, China
  12. Analyzing forest effects on runoff and sediment production using leaf area index
  13. Effects of heat softening on initiation of landslides
  14. Characteristics of viscous debris flow in a drainage channel with an energy dissipation structure
  15. Experimental investigation on the relevance of mechanical properties and porosity of sandstone after hydrochemical erosion
  16. Micromorphology of solonetzic horizons as related to environmental events in the Caspian Lowland
  17. Non-point-source nitrogen and phosphorus loadings from a small watershed in the Three Gorges Reservoir area
  18. Temporal variations in carbon stock of Pinus roxburghii Sargent forests of Himachal Pradesh, India
  19. A public Cloud-based China’s Landslide Inventory Database (CsLID): development, zone, and spatiotemporal analysis for significant historical events, 1949-2011

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