山地城市建设用地增长的坡度梯度效应——以贵阳市为例
彭秋志(1982- ),男,云南文山人,博士,讲师,主要从事基于RS与GIS技术的土地资源问题研究。E-mail: pengqiuzhi@kust.edu.cn |
收稿日期: 2021-03-22
修回日期: 2021-06-23
网络出版日期: 2022-09-28
基金资助
国家自然科学基金项目(41961039)
Relationship between construction land and slope in rapidly expanding mountain cities: A case study in Guiyang, China
Received date: 2021-03-22
Revised date: 2021-06-23
Online published: 2022-09-28
山地城市快速扩张致使其建设用地爬坡现象日趋普遍,深入认识该现象将有助提高山区国土空间管控科学性。以中国西南典型山地城市贵阳为例,利用数字高程模型和2000—2020年五期建设用地数据,构建建设用地密度、建设用地爬坡热度等指标,基于网格单元和坡度区段单元开展统计分析,探究该市建设用地增长的坡度梯度效应。结果表明:(1)建设用地面积的增长总体伴随着建设用地平均坡度的趋陡,各相邻时段新增建设用地面积先增大后减小,但新增建设用地平均坡度却一直在变陡;(2)各时期建设用地的现状密度和新增密度均随坡度上升而减小,在坡度梯度上体现出强烈的“择平而建”效应;(3)建设用地密度对建设用地爬坡热度有显著线性影响,且该影响随着背景地面平均坡度上升而增强。研究认为,建设用地爬坡现象通常更多出现在建设用地加密时期,这有利于促进山地城市实现更为集约紧凑的空间增长。
彭秋志 , 马少华 , 邓启辉 , 马经纬 . 山地城市建设用地增长的坡度梯度效应——以贵阳市为例[J]. 自然资源学报, 2022 , 37(7) : 1865 -1875 . DOI: 10.31497/zrzyxb.20220714
With the rapid urbanization, the land utilization rate in the mountainous areas has been increasing. Therefore, we should deepen our understanding of the construction land expansion in mountain cities, so as to carry out more scientific management of land use in mountainous areas. This paper studied the slope gradient effect of construction land growth in Guiyang, a typical mountain city in Southwest China, using digital elevation model (DEM) and construction land datasets of 2000, 2005, 2010, 2015 and 2020, which was integrated with zonal statistics approaches based on spatial statistics unit of kilometer grid and slope section with one degree interval. Combined with the information of construction land density and slope, we propose a novel method to quantify the spatial pattern of construction land climbing. The research was designed to address three research questions: Is there a synergistic relationship between the area of construction land and the average slope of construction land? What are the distribution and change characteristics of construction land density on the slope gradient? What is the relationship between the density of construction land and the heat of construction land climbing? The results showed that: (1) The total area of construction land is positively correlated with the average slope of construction land, both of which increase gradually across the entire study period. However, the average slope of new construction land gradually becomes steeper among four neighboring periods, while the area of new construction land turns from increasing to decreasing, implying that they are not synchronous. (2) The density of construction land in each period decreased with the increase of slope, no matter in one period or in the other four periods. (3) The density of construction land has a significant impact on the heat of construction land climbing, and this influence increases as the average slope of the background ground rises. This paper suggests that the phenomenon of construction land climbing would promote the intensification and compactness of construction land in mountain cities.
Key words: mountain city; urban expansion; construction land; slope; Guiyang city
表1 分区县各变化时段新增建设用地面积及其平均坡度Table 1 Area of newly-added construction land and average slope |
地区 | 2000—2005年 | 2005—2010年 | 2010—2015年 | 2015—2020年 | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|
面积/km2 | 坡度/(°) | 面积/km2 | 坡度/(°) | 面积/km2 | 坡度/(°) | 面积/km2 | 坡度/(°) | ||||
南明区 | 4.4 | 6.5 | 10.2 | 7.3 | 20.6 | 8.6 | 10.8 | 8.4 | |||
云岩区 | 4.0 | 8.5 | 7.6 | 9.6 | 13.8 | 12.2 | 3.6 | 12.5 | |||
花溪区 | 5.0 | 5.5 | 22.1 | 6.2 | 65.9 | 6.5 | 27.1 | 6.8 | |||
乌当区 | 3.1 | 5.9 | 7.3 | 7.4 | 15.6 | 8.8 | 5.9 | 8.7 | |||
白云区 | 4.0 | 4.5 | 13.3 | 4.3 | 31.3 | 4.9 | 10.2 | 5.7 | |||
观山湖区 | 5.0 | 5.0 | 20.9 | 6.0 | 34.6 | 6.9 | 8.8 | 7.8 | |||
开阳县 | 1.1 | 6.0 | 5.6 | 7.4 | 10.3 | 8.4 | 5.8 | 9.0 | |||
息烽县 | 1.1 | 7.3 | 4.1 | 7.7 | 5.5 | 8.4 | 3.3 | 9.4 | |||
修文县 | 1.8 | 4.0 | 4.3 | 4.6 | 15.9 | 4.9 | 6.9 | 5.0 | |||
清镇市 | 2.3 | 5.3 | 10.2 | 5.4 | 29.3 | 6.2 | 10.2 | 7.0 | |||
全贵阳市 | 31.9 | 5.8 | 105.7 | 6.4 | 242.9 | 7.0 | 92.5 | 7.4 |
图8 背景坡度分组下2020年建设用地坡度份额与建设用地密度关系Fig. 8 Relationship between construction land slope share and construction land density in 2020 under background slope grouping |
表2 背景坡度分组下各年份拟合参数Table 2 Fitting parameters for each year under background slope grouping |
年份 | 0~5° | 5~10° | 10~15° | >15° | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|
R2 | a | R2 | a | R2 | a | R2 | a | ||||
2000 | 0.898 | 0.007 | 0.943 | 0.009 | 0.893 | 0.013 | 0.896 | 0.016 | |||
2005 | 0.895 | 0.005 | 0.941 | 0.007 | 0.891 | 0.010 | 0.906 | 0.013 | |||
2010 | 0.900 | 0.003 | 0.935 | 0.004 | 0.912 | 0.006 | 0.923 | 0.008 | |||
2015 | 0.872 | 0.001 | 0.923 | 0.002 | 0.912 | 0.003 | 0.944 | 0.004 | |||
2020 | 0.859 | 0.001 | 0.920 | 0.002 | 0.916 | 0.003 | 0.944 | 0.004 |
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