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1.
中国分县生态承载力供需平衡空间格局分析(英文) 总被引：5，自引：1，他引：4
A balanced ecological carrying capacity and its understanding are important to achieve sustainable development for human kind.Here,the concept of ecological carrying capacity has been used for measuring the dependencies between human and nature.China’s ecological balance between supply and demand has become a global concern and is widely debated.In this study the ’Ecological Footprint’ method was used to analyze the supply-demand balance of China’s ecological carrying capacity.Firstly,the ecological supply and demand balance was calculated and evaluated,and secondly,the ecological carrying capacity index (ECCI) was derived for each county of China in 2007,and finally this paper systematically evaluated the ecological carrying capacity supply-demand balance of China.The results showed that ecological deficit appeared to be the main characteristic of ecological carrying capacity supply-demand balance in 2007 of China at county scale.In general,more than four-fifths of the Chinese population was concentrated in less than one-third of the land area and more than two-thirds of the land area was inhabited by less than one-fifth of the population.The spatial distribution of the ecological carrying capacity demand-supply was unbalanced ranging from significant overloading to affluence from southeastern to northwestern part of China.It appeared to be more dominant in regions located at coastal areas which are attracted by migrants and had a generally higher population density.Along with the rapid development and urbanization trends in China,ecological deficits in these regions will become more severe. 相似文献
2.
近30年中国东北地区玉米种植体系的时空动态分析(英文) 总被引：5，自引：1，他引：4
Understanding crop patterns and their changes on regional scale is a critical requirement for projecting agro-ecosystem dynamics. However, tools and methods for mapping the distribution of crop area and yield are still lacking. Based on the cross-entropy theory, a spatial production allocation model(SPAM) has been developed for presenting spatio-temporal dynamics of maize cropping system in Northeast China during 1980–2010. The simulated results indicated that(1) maize sown area expanded northwards to 48°N before 2000, after that the increased sown area mainly occurred in the central and southern parts of Northeast China. Meanwhile, maize also expanded eastwards to 127°E and lower elevation(less than 100 m) as well as higher elevation(mainly distributed between 200 m and 350 m);(2) maize yield has been greatly promoted for most planted area of Northeast China, especially in the planted zone between 42°N and 48°N, while the yield increase was relatively homogeneous without obvious longitudinal variations for whole region;(3) maize planting density increased gradually to a moderately high level over the investigated period, which reflected the trend of aggregation of maize cultivation driven by market demand. 相似文献
3.
《地理学报(英文版)》2019,(4)
Topographical relief is a key factor that limits population distribution and economic development in mountainous areas. The limitation is especially apparent in the mountain-plain transition zone. Taking the transition zone between the Qinling Mountains and the North China Plain(i.e. the mountainous area in western Henan Province) as an example and based on the 200-m resolution DEM data, we used the mean change-point analysis to determine the optimal statistical unit for topographical relief, and thereafter extracted the relief degree. Taking the 1:100,000 land use data, township population and county-level industrial data, population and economic spatial models were constructed, and 200-m resolution grid population and economic density maps were generated. Afterwards, statistical analysis was carried out to quantitatively reveal the impact of topographical relief on population and economy. In addition, the impacts of other topographical factors were discussed. The results showed the following.(1) The relief degree in western Henan is generally low, where 58.6% of the regional topography does not exceed half the height of a reference mountain(relative elevation ≤250 m). Spatially, the relief degree is high in the west while low in the east, and high in the middle while low in the north and south. There is a positive correlation between relief degree and elevation, and a much stronger correlation between relief degree and slope.(2) The linear fitting degree between the population and economic validation data and the corresponding simulation data are 0.943 and 0.909, respectively, indicating that the spatialized results can reflect the actual population and economic distribution.(3) The impact of topographical relief on population and economy was stronger than that of other topographical factors. The relief degree showed a good logarithmic fit relationship with population density(0.911) and economic density(0.874). Specifically, 88.65% of the population lives in areas where the topographical relief is ≤0.5 and 88.03% of the gross regional product was from areas where the relief is ≤0.3. Compared with the population distribution, the economic development showed an obvious agglomeration trend towards low relief areas. 相似文献
4.
According to the connotation and structure of science and technology resources and some relevant data of more than 286 cities at prefecture level and above during 2001–2010, using modified method—Data Envelopment Analysis(DEA), science and technology(ST) resource allocation efficiency of different cities in different periods has been figured out, which, uncovers the distributional difference and change law of ST resource allocation efficiency from the time-space dimension. Based on that, this paper has analyzed and discussed the spatial distribution pattern and evolution trend of ST resource allocation efficiency in different cities by virtue of the Exploratory Spatial Data Analysis(ESDA). It turned out that:(1) the average of ST resource allocation efficiency in cities at prefecture level and above has always stayed at low levels, moreover, with repeated fluctuations between high and low, which shows a decreasing trend year by year. Besides, the gap between the East and the West is widening.(2) The asymmetrical distribution of ST resource allocation efficiency presents a spatial pattern of successively decreasing from Eastern China, Central China to Western China. The cities whose ST resource allocation efficiency are at higher level and high level take on a cluster distribution, which fits well with the 23 forming urban agglomerations in China.(3) The coupling degree between ST resource allocation efficiency and economic environment assumes a certain positive correlation, but not completely the same. The differentiation of ST resource allocation efficiency is common in regional development, whose existence and evolution are directly or indirectly influenced by and regarded as the reflection of many elements, such as geographical location, the natural endowment and environment of ST resources and so on.(4) In the perspective of the evolution of spatial structure, ST resource allocation efficiency of the cities at prefecture level and above shows a notable spatial autocorrelation, which in every period presents a positive correlation. The spatial distribution of ST resource allocation efficiency in neighboring cities seems to be similar in group, which tends to escalate stepwise. Meanwhile, the whole differentiation of geographical space has a diminishing tendency.(5) Viewed from LISA agglomeration map ofST resource allocation efficiency in different periods, four agglomeration types have changed differently in spatial location and the range of spatial agglomeration. And the continuity of ST resource allocation efficiency in geographical space is gradually increasing. 相似文献
5.
Based on the hydrographic data in austral summer during the 22nd Antarctic Expedition of China(2005/2006),some features can be found about the northern margin of Emery ice shelf as follows.The heat content in the surface layer(0-50 m) at the eastern end and the western end of the ice-shelf margin is much higher than that at the middle.The upper mixing-layer depth and the seasonal thermocline depth at the middle of the ice-shelf northern margin are much shallower than those at the both ends.However there is much less difference between the middle and the ends in the bottom layer.The remote sensing photos show that the inhomogeneity in the surface-layer water is closely related to the spatial distribution of the floes and polynia in the area. 相似文献
6.
中国流动人口地域类型——划分方法及空间分布(英文) 总被引：3，自引：3，他引：0
With the rapid increase of the number and influence of floating population in China,it is urgently needed to understand the regional types of China’s floating population and their spatial characteristics. After reviewing the current methods for identifying regional types of floating population,this paper puts forward a new composite-index identification method and its modification version which is consisted of two indexes of the net migration rate and gross migration rate. Then,the traditional single-index and the new composite-index identification methods are empirically tested to explore their spatial patterns and characteristics by using China’s 2000 census data at county level. The results show:(1) The composite-index identification method is much better than traditional single-index method because it can measure the migration direction and scale of floating simultaneously,and in particular it can identify the unique regional types of floating population with large scale of immigration and emigration. (2) The modified composite-index identification method,by using the share of a region’s certain type of floating population to the total in China as weights,can effectively correct the over-or under-estimated errors due to the rather large or small total population of a region. (3) The spatial patterns of different regional types of China’s floating population are closely related to the regional differentiation of their natural environment,population density and socio-economic development level. The three active regional types of floating population are mainly located in the eastern part of China with lower elevation,more than 800 mm precipitation,rather higher population densities and economic development levels. 相似文献
7.
历史时期中国重大自然灾害时空分异特征(英文) 总被引：4，自引：0，他引：4
Based on historical documents and records this paper analyzes the characteristics of frequency and distribution of major disasters that took place in the history of China. The findings show that occurrences of different types of disasters varied and spatial pattern at provincial level are significantly different as well. The results also indicate that there is a strong relationship between type of disasters and spatial distribution and that the spatial pattern of losses was not the same as that of the frequency. The reasons are: (1) the hazard-formative environments which, to a large extent, determine the spatial pattern of the disasters are significantly different; (2) the losses caused by natural disasters were closely related to the concentration of economy and population. Number of deaths was usually large in areas where agriculture, culture and business were relatively developed. The spatial pattern of disaster losses is an evitable result of uneven economic development in the history of China. 相似文献
8.
《地理学报(英文版)》2017,(3)
To investigate the diurnal variation of summer precipitation in the Qilian Mountains in the northeast Tibetan Plateau,the hourly precipitation amount for this region during the summers of 2008–2014 are analyzed using an hourly merged precipitation product at 0.1°×0.1° resolution.The main results are as follows.(1) The spatial distribution and temporal variation of mean hourly precipitation amount and frequency are generally similar and hourly precipitations in the eastern and middle portions are larger and more frequent than that in the western portion.The high value area of precipitation intensity is obviously different from that of precipitation amount and frequency.(2) The spatial distribution of daytime precipitation is generally similar to that of nighttime precipitation,and the daytime precipitation is heavier than the nighttime precipitation.(3) The change rate of precipitation has a maximum at 20:00 Beijing time,and a minimum at 12:00.The hourly precipitation amount significantly correlated with frequency,especially for the middle and eastern portions. 相似文献
9.
基于GIS的中国人口重心的密度分级与曲线特征 总被引：1，自引：1，他引：0
In this paper, with the spatial analysis functions in ArcGIS and the county-level census data of 2000 in China, the population density map was divided and shown by classes, meanwhile, the map system of population distribution and a curve of population centers were formed; in accordance with the geographical proximity principle, the classes of population densities were reclassified and a population density map was obtained which had the spatial clustering characteristic. The multi-layer superposition based on the population density classification shows that the population densities become denser from the Northwest to the Southeast; the multi-layer clustering phenomenon of the Chinese population distribution is obvious, the populations have a water-based characteristic gathering towards the rivers and coastlines. The curve of population centers shows the population densities transit from the high density region to the low one on the whole, while in low-density areas there are relatively dense areas, and in high-density areas there are relatively sparse areas. The reclassification research on the population density map based on the curve of population centers shows that the Chinese population densities can be divided into 9 classes, hereby, the geographical distribution of Chinese population can be divided into 9 type regions: the concentration core zone, high concentration zone, moderate concentration zone, low concentration zone, general transitional zone, relatively sparse area, absolute sparse area, extreme sparse area, and basic no-man's land. More than 3/4 of the population of China is concentrated in less than 1/5 of the land area, and more than half of the land area is inhabited by less than 2% of the population, the result reveals a better space law of China’s population distribution. 相似文献
10.
JianZhong Xu ShiChang Kang ShuGui Hou QiangGong Zhang Jie Huang CunDe Xiao JiaWen Ren DaHe Qin 《寒旱区科学》2016,8(1):9-21
From 2008 to 2010,a total of 15 snow pit samples were collected from 13 mountain glaciers in western China.In this study these samples are used to determine the spatial distribution of insoluble particle concentrations and dust deposition fluxes in western China.The results show that the mass concentrations of insoluble particles exhibit high spatial variation and strongly decrease(by a factor of approximately 50) from the north(Tienshan Mountains) to the south(Himalayas).However,the insoluble particles concentrations at the southeastern Tibetan Plateau(TP) sites are also high and approximately 30 times greater than those in the Himalayas.The spatial distribution of the dust flux is similar to that of the mass concentrations;however,the high dust deposition rate in the southeastern TP is very significant as a result of the extensive snow accumulation(precipitation) in this region.The average sizes of the insoluble particles at each site generally exhibit bimodal distributions with peaks at approximately 5 μm and 10 μm,which can be explained as resulting from dust emissions from regional and local sources,respectively.The enrichment factors for most of the elements measured in insoluble particles are less than 10 at all of the study sites,indicating primarily crustal sources.However,the sites located in the peripheral mountains of western China,such as the Tienshan Mountains and the Himalayas,are characterized by high levels of certain enrichment elements(e.g.,Cu,Zn,Cr,and V) indicative of sources related to the long-range transport of pollutants. 相似文献
11.
The relief degree of land surface (RDLS) is an important factor for describing the landform at macro-scales. This study defines a concept for RDLS and applies the concept for population distribution study of the entire country. Based on the concept and macro-scale digital elevation model datum and ARC/INFO software, the RDLS at a 10 km×10 km grid size of China is extracted. This paper depicts systemically the spatial distributions of RDLS through analyzing the ratio structure and altitudinal characters of RDLS in China. The con-clusions are drawn as follows: the RDLS in more than 63% of the area is less than one (1) (relative altitude is less than 500 m), reflecting the fact that most of RDLS in China is low. In general, the RDLS in the west is larger than that in the east and so is the south than that of the north in China. The RDLS decreases with the increase of longitude and latitude and the change of RDLS at the latitudes of 28°N, 35°N, 42°N, as well as at the longitudes of 85°E, 102°E, 115°E could reflect the three major ladders of China. In the vertical direction, the RDLS increases with the increase of altitude. Analysis of the correlation between RDLS and population distribution in China and its regional difference shows that the R2 value between RDLS and population density is 0.91 and RDLS is an important factor influencing the spatial distribution of population. More than 85% of the people in China live in areas where the RDLS is less than one (1), while the population in areas with RDLS greater than 3 accounts only for 0.57% of the total. The regional difference of correlation between RDLS and population within China is significant and such correlation is significant in Central China and South China and weak in Inner Mongolia and Tibet. 相似文献
12.
中国地形起伏度及其与人口分布的相关性 总被引：68，自引：15，他引：53
基于人居环境自然评价的需要, 运用GIS 技术, 采用窗口分析等方法, 提取了基于栅 格尺度(10 km×10 km) 的中国地形起伏度, 并从比例结构、空间分布和高度特征3 个方面系 统分析了中国地形起伏度的分布规律及其与人口分布的相关性。研究表明: 中国的地形起伏度以低值为主, 63%的区域低于1 (相对高差≤500 m); 空间分布呈现西高东低、南高北低的格局; 随着经度和纬度增高, 地形起伏度呈逐渐下降趋势, 28oN、35oN、42oN 纬线和85oE、102oE、115oE 经线上的地形起伏度符合中国三大阶梯的地貌特征; 随着海拔高度增加, 地形 起伏度呈现逐渐升高趋势。实证分析表明: 中国的地形起伏度与人口密度有较好的对数拟合关系, 拟合度高达0.91; 全国85%以上的人口居住在地形起伏度小于1 的地区, 在地形起伏度大于3 的地区居住的人口总数只占全国0.57%。中国地形起伏度与人口分布的相关性区域差异显著, 东北、华北、华中和华南等地相关性显著, 内蒙古与青藏地区几乎不存在相关性。 相似文献
13.
基于栅格的豫西山区地形起伏特征及其对人口和经济的影响 总被引：6，自引：0，他引：6
地形起伏是约束山区人口分布和经济发展的关键因素,尤其在山地平原过渡带其约束作用更为显著。以位于秦岭-黄淮平原过渡带的豫西山区为例,基于200 m分辨率DEM数据,采用均值变点法确定地形起伏度的最佳统计单元,并提取地形起伏度;以1∶10万土地利用、乡镇人口和县域各产业数据为基础,建立人口和经济空间化模型,同时生成200 m分辨率的栅格人口和经济密度图;在系统分析地形起伏度、人口和经济密度空间分布规律的基础上,借助统计分析方法基于栅格单元定量揭示了地形起伏度对人口和经济的影响,并与其他地形因子的影响进行对比分析。结果表明：① 豫西山区地形起伏度以低值为主,58.6%的区域地形起伏度小于等于0.5个基准山体的高度（相对高差≤ 250 m）;空间上呈西高东低、中间高南北低的格局,与海拔、坡度均呈较强的正相关,且与坡度的相关性更大。② 被选作验证的人口和经济数据与对应模拟值的线性拟合度分别为0.943和0.909,表明空间化结果能反映人口和经济分布的实际状况。③ 地形起伏度对人口和经济的影响强于其他地形因子的影响,与人口密度和经济密度呈较好的对数拟合关系,拟合度分别为0.911和0.874;豫西山区88.65%的人口居住在地形起伏度不超过0.5的地区,88.03%的生产总值分布在地形起伏度不超过0.3的地区。相对人口分布,研究区的经济发展向地形起伏度低值区的集聚态势更加明显。 相似文献
14.
1IntroductionInrecentyears,studyonglobalchangehasbecomethefocus,onwhichstresshasbeenlaidbytodayhumansociety.Inordertodealwithseriesofenvironmentalproblemssuchasdegradationoflandresources,globalwarming,destructionofozonosphereandsoon,andassurethestabilizationandsustainabledevelopmentofworldeconomy,IGBPhasestablishedthestudyframeforglobalchange.Withavastrangeofstudy,researchonglobalchangehasbroughtforwardagreatdealofimportantscientificquestionsrelatedtofeasibilityforhumanelivingoftheEarth.Inth… 相似文献
15.
Spatio-temporal analysis of the geographical centroids for three major crops in China from 1949 to 2014 总被引：3，自引：1，他引：2
Lingling Fan Shefang Liang Hao Chen Yanan Hu Xiaofei Zhang Zhenhuan Liu Wenbin Wu Peng Yang 《地理学报(英文版)》2018,28(11):1672-1684
Spatial distribution changes in major crops can reveal important information about cropping systems. Here, a new centroid method that applies physics and mathematics to spatial pattern analysis in agriculture is proposed to quantitatively describe the historical centroids of rice, maize and wheat in China from 1949 to 2014. The geographical centroids of the rice area moved 413.39 km in a 34.32° northeasterly (latitude 3.08°N, longitude 2.10°E) direction at a speed of 6.36 km/year from central Hunan province to Hubei province, while the geographical centroids of rice production moved 509.26 km in the direction of 45.44° northeasterly (latitude 3.22°N, longitude 3.27°E) at a speed of 7.83 km/year from central Hunan province to Henan province. The geographical centroids of the maize area and production moved 307.15 km in the direction of 34.33° northeasterly (latitude 2.29°N, longitude 1.56°E) and 308.16 km in the direction of 30.79° northeasterly (latitude 2.39°N, longitude 1.42°E), respectively. However, the geographical centroids of the wheat area and production were randomly distributed along the border of Shanxi and Henan provinces. We divided the wheat into spring wheat and winter wheat and found that the geographical centroids of the spring wheat area and production were distributed within Inner Mongolia, while the geographical centroids of winter wheat were distributed in Shanxi and Henan provinces. We found that the hotspots of crop cultivation area and production do not always change concordantly at a larger, regional scale, suggesting that the changing amplitude and rate of each crops’ yield differ between different regions in China. Thus, relevant adaptation measures should be taken at a regional level to prevent production damage in those with increasing area but decreasing production. 相似文献
16.
基于乡镇尺度的中国25省区人口分布特征及影响因素 总被引：16，自引：2，他引：14
人口空间分布具有典型的尺度特征,精细尺度的人口分布是当前人口地理学研究的热点和难点。乡镇（街道）是中国人口普查数据公开发布的最小行政单元,乡镇级人口密度计算及其分布特征研究能够更客观、精细地刻画中国人口分布的空间格局和态势,为促进中国人口的合理优化布局提供科学依据和决策支持。本文收集处理了2000年中国25个省（直辖市、自治区）的乡镇（街道）级行政边界数据,基于第五次人口普查乡镇（街道）人口统计数据,计算了乡镇级平均人口密度。采用Lorenz曲线、空间分析及样带分析的方法,分析了研究区乡镇（街道）人口分布的疏密结构、空间集聚性、纬向和经向规律。利用相关分析和逐步回归分析,分省探究了地形起伏度、水网密度、路网密度及社会经济发展水平（利用夜间灯光指数表征）等4个因素对于乡镇级人口分布的影响。研究表明：① 乡镇级平均人口密度能够有效区分出县域内部的人口密度高低差异,整体不均衡性高于基于县级平均人口密度的研究结果;② 乡镇（街道）人口分布总体规律是西北稀疏东南密集,同时,东南密中有疏,西北疏中有密;③ 乡镇（街道）人口分布的经纬向规律变异较大,既受中国三级阶梯地貌大势的影响,也受局部微地形及区域中心城市的影响,并和海岸线、交通枢纽及大江大河的分布具有一定的空间耦合性。④ 乡镇级平均人口密度与地形起伏度、水网密度、路网密度及夜间灯光指数等显著相关,省级平均相关系数分别为-0.56、0.28、0.61、0.69。⑤ 在乡镇尺度上,地形条件及区域发展水平对辽、吉、京、津、沪、冀、豫、陕、晋、鲁、皖、苏、湘、鄂、赣、浙、闽、粤、琼等省份的人口分布具有较强的决定作用。⑥ 对于藏、青、蒙、滇、黔等5省或自治区,需要引入更多的自然环境及社会因素来解释其人口分布的特殊规律。本研究扩充了中国人口地理学的研究尺度和维度,并引入了新的定量分析和空间分析方法,所构建的覆盖中国25省（直辖市、自治区）的乡镇（街道）级人口分布科学数据集丰富了中国人口地理学的2000年本底数据资源。 相似文献
17.
昆明滇池对其周围地区温度的贡献及其特征 总被引：1，自引：0，他引：1
本文以订正和消除方法,显示出滇池(湖泊)对其周围的各项温度贡献值即湖泊温效(ΔT)并据此讨论盆湖平填区与山麓带的各项湖泊温效的时、空分布特征。 相似文献
18.
Hongya Wang Hongyan Liu Yanhua Liu Haiting Cui Niels Abrahamsen 《Journal of Paleolimnology》2010,43(2):345-367
The Qinling Mountain Range (33°–34°30′N, 107°–111°E; 3,767 m a.s.l.) lies south of the Chinese Loess Plateau and functions
as the boundary between ‘north’ and ‘south’ China. Taibai Mountain (33°41′–34°10′N, 107°19′–107°58′E; 3,767 m a.s.l.) is the
central massif and highest part of the range and is the highest mountain in eastern and central China, east of 105°E. It is
also one of two mountains higher than the modern climatic timberline and the only one where high alpine lakes (>2,500 m a.s.l.)
exist in eastern and central China. Sediments were recovered from Foye Chi (33°57′N, 107°44′E; 3,410 m a.s.l.), a small lake
on the southern slope of the mountain, and measured for magnetic properties. Chronological control was achieved with AMS 14C dating. Combined with analyses of particle-size, TOC, C/N, δ13Corg and pollen in these sediments, and magnetic properties of catchment soils, the mineral-magnetic data reveal late Holocene
palaeoenvironmental changes on the high-altitude southern slope of Taibai Mountain. Climate gradually ameliorated about 2,300 cal yr BP
and warm and wet conditions occurred afterwards, culminating from 1,700 to 1,510 cal yr BP. The climate began to deteriorate
at 1,510 cal yr BP, but was still warmer and wetter than present until ~663 cal yr BP. Cool, arid conditions peaked and were
cooler and drier than the present at 663–290 cal yr BP, coincident with the Little Ice Age. Climate became warmer and more
humid again after 290 cal yr BP. Data from these less anthropologically-disturbed alpine-lake sediments provide a record of
late Holocene palaeoenvironmental change that supplements information from historical documents and literature for eastern
and central China. 相似文献