人类活动强度是地理学、生态学和自然资源学等多学科研究中的重要参数,定量化和空间化是当前人类活动强度研究的重点和难点。本文针对现有的人类活动强度定量化和空间化方法的不足,提出了一种以统计学和空间分析方法的空间模拟方法,对典型的南方丘陵区衡阳盆地人类活动强度的空间分布进行了定量研究。结果表明:衡阳盆地工业活动高强度区呈现一极一带分布,衡阳市市区为极强区,祁东县、常宁市和耒阳市形成了一条南北走向的较强带,工业活动低强度区呈以衡阳市市区为中心的环状分布;农业活动强度分布呈西北向东南逐渐减弱的趋势;交通活动整体分布较为均匀,高值区主要分布在国道和省道沿线;总的人类活动强度整体表现不强,但区域差异明显,衡阳市市区及其周边区域人类活动强度最大,低强度区位于衡东县内。根据研究结果,应采取发展北部工业、加强市区对周边区域工业带动和控制西北部农业等调控策略。
Abstract
Quantification and spatialization of human activity intensity are the key and difficult problems of geography,ecology and resource science as human activities are considered.There are two kinds of methods to resolve these problems,the first is by statistic data and statistical methods,and the other is by geography information data(such as traffic data) and spatial analysis methods,but the satisfied result can not be obtained from these methods.A new method that combines statistic method and GIS spatial analysis was proposed,and it was used to simulate spatial distribution of human activity intensity of Hengyang basin in southern China.The main conclusions were:(1) there are two regions of high human industrial activity intensity,one is the urban area of Hengyang city and the other is west-east band composed of Qidong,Changning and Leiyang,and the low human industrial activity intensity looked like a circle that is composed of Hengnan,Hengshan,Hengyang and Hengdong;(2) the agricultural activities decreased from north-west to south-east;(3) the difference of traffic activities of different regions was small;and(4) the total human activity intensity of the study area was small but the difference among regions is obvious,the area with the maximum value located in urban region of Hengyang city and the surrounding of it,and Hengdong got the minimum value.Some tactics should be taken to adjust human activities in the study area,such as developing industry in northern region,strengthening the impact of urban region on neighboring regions,and controlling the practice of agricultural production in north-west regions.
关键词
人类活动强度 /
南方丘陵区 /
衡阳盆地 /
空间模拟
{{custom_keyword}} /
Key words
human activity intensity /
hilly red soil region of southern China /
Hengyang Basin /
spatial simulation
{{custom_keyword}} /
{{custom_sec.title}}
{{custom_sec.title}}
{{custom_sec.content}}
参考文献
[1]De la T o rre S,Snow don C T,Be jarano M.E ffects o f Hum an A ctiv ities on W ild Pygmy t M a rmo sets in Ecuador ianAm azon ia[J].B io log ical Conserva tion,2000,94:153-163.
[2]Quan R C,W en X J,Y ang X J.E ffec t o fHuman A ctiv itieson M igratory W aterb irds at Lash ihai L ake[J].B io log ica lConservation,2002,108:273-279.
[3]林学钰,方燕娜,廖资生,等.全球气候变暖和人类活动对地下水温度的影响[J].北京师范大学学报,2009,10(45):452-257.
[4]周洪建,王静爱,岳耀杰,等.人类活动对植被退化/恢复影响的空间格局以陕西省为例[J].生态学报,2009,29(9):4847-4846.
[5]纲胜,夏军,万东晖.气候变化及人类活动影响下的潮白河月水量平衡模拟[J].自然资源学报,2006,21(1):85-90.
[6]魏建兵,肖笃宁,解伏菊.人类活动对生态环境的影响评价与调控原则[J].地理科学进展,2006,25(2):36-45.
[7]段建军,王彦国,王晓风,等.1957-2006年塔里木河流域气候变化和人类活动对水资源和生态环境的影响[J].冰川冻土,2009,31(5):781-791.
[8]樊哲文,刘木生,沈文清,等.江西省生态脆弱性现状G IS模型评价[J].地球信息科学学报,2009,11(2):231-238.
[9]文英.人类活动强度定量评价方法的初步探讨[J].科学对社会的影响(中文版),1998(4):55-60.
[10]曾辉,刘国军.基于景观结构的区域生态风险分析[J].中国环境科学,1999,19(5):454-457.
[11]李香云,王立新,章予舒.西北干旱区土地荒漠化中人类活动作用及其指标选择[J].地理科学,2004,24(1):68-75.
[12]李香云,王立新,章予舒.干旱区人类活动指数的动态研究以塔里木河流域1978-2000年县级区为例[J].兰州大学学报(自然科学版),2004,40(4):106-111.
[13]张翠云,王昭.黑河流域人类活动强度的定量评价[J].地理科学进展,2004,19(增刊):386-390.
[14]黄领梅,沈冰.干旱区人类活动干扰程度定量评估研究[J].西安理工大学学报,2009,25(4):425-429.
[15]王金哲,张光辉,聂振龙,等.滹沱河流域平原区人类活动强度的定量评价[J].干旱区资源与环境,2009,23(10):41-45.
[16]徐志刚,庄大方,杨琳.区域人类活动强度定量模型的建立与应用[J].地球信息科学学报,2009,11(4):452-460.
[17]胡志斌,何兴元,李月辉,等.岷江上游地区人类活动强度及其特征[J].生态学杂志,2007,26(54):539-543.
[18]田亚平,刘沛林,郑文武.南方丘陵区的生态脆弱度评估以衡阳盆地为例[J].地理研究,2005,24(6):843-852.632
{{custom_fnGroup.title_cn}}
脚注
{{custom_fn.content}}
基金
国家自然科学基金项目(40971067);湖南省资源环境管理与区域可持续发展科技创新团队研究项目;湖南省教育厅课题成果(08C154)
{{custom_fund}}