Impacts of rapid land use change on soil infiltration in an arid desert area

doi:10.7522/j.issn.1000-694X.2019.00097

Journal of Desert Research ›› 2020, Vol. 40 ›› Issue (4): 146-153.DOI: 10.7522/j.issn.1000-694X.2019.00097

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Impacts of rapid land use change on soil infiltration in an arid desert area

Runxia Zhang¹^,²^,³(), Xueyong Zhao¹(), Jing Li², Wenqiang Lv², Yuanyuan Chai¹^,²^,³, Hongqing Yue²

^1.Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
^2.Gansu Institute of Soil and Water Conservation Science, Lanzhou 730000, China
^3.University of Chinese Academy of Sciences, Beijing 100049, China

Received:2019-08-31 Revised:2019-10-25 Online:2020-08-20 Published:2020-09-01
Contact: Xueyong Zhao

Abstract

Abstract:

Studying on soil infiltration and its influence factors in different land use types are beneficial to urban runoff regulation and land management. This research selected six land use types (e.g. natural forest, artificial forest, natural grassland, land to be constructed, cropland, abandoned land) and observed the process of soil infiltration using disc permeameter. Correlation analysis and principal component analysis were used to establish the relationship between soil infiltration and soil properties. The results showed that land use change could increase soil bulk density and sand content, while decrease total porosity and soil saturated water content during urbanization. The parameters of soil infiltration of land to be constructed and artificial forest were significant lower than those of the other land use types. Soil infiltration was positively correlated with soil organic matter, total porosity, soil saturated water content and silt content, while negatively correlated with soil bulk density, sand and clay content. The shift of the other land use types to constructed land and building area had altered soil physicochemical properties and affected soil infiltration.

Key words: rapid urbanization, Lanzhou New District, soil infiltration, arid desert area

CLC Number:

S152.7

Runxia Zhang, Xueyong Zhao, Jing Li, Wenqiang Lv, Yuanyuan Chai, Hongqing Yue. Impacts of rapid land use change on soil infiltration in an arid desert area[J]. Journal of Desert Research, 2020, 40(4): 146-153.

Figures/Tables 7

References 44

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土地利用类型	砂粒 /%	粉粒 /%	黏粒 /%	容重 /(g·cm^-3)	有机质 /(g·kg^-1)	总孔隙度 /%	初始土壤含水量/%	饱和含水量/%
人工生态林L1	19. 89^a	61.61^ab	18.50^a	1.18^a	27.00^a	55.81^ac	17.59^a	49.44^a
人工生态经济混交林L2	18.57^a	55.84^b	25.59^c	1.33^b	25.53^a	50.74^a	23.97^b	37.99^b
自然草地L3	16.73^a	67.93^a	15.35^a	1.19^a	28.36^a	54.68^ac	7.03^c	51.95^a
待建地L4	41.79^b	38.90^c	19.31^ab	1.56^c	15.70^b	43.33^b	7.83^c	27.66^c
农田L5	18.36^a	59.42^ab	22.22^bc	1.08^d	37.30^c	60.15^c	9.38^c	56.72^a
撂荒地L6	18.24^a	57.51^ab	24.24^c	1.22^a	27.78^a	54.81^ac	9.45^c	50.41^a

土地利用类型	砂粒 /%	粉粒 /%	黏粒 /%	容重 /(g·cm^-3)	有机质 /(g·kg^-1)	总孔隙度 /%	初始土壤含水量/%	饱和含水量/%
人工生态林L1	19. 89^a	61.61^ab	18.50^a	1.18^a	27.00^a	55.81^ac	17.59^a	49.44^a
人工生态经济混交林L2	18.57^a	55.84^b	25.59^c	1.33^b	25.53^a	50.74^a	23.97^b	37.99^b
自然草地L3	16.73^a	67.93^a	15.35^a	1.19^a	28.36^a	54.68^ac	7.03^c	51.95^a
待建地L4	41.79^b	38.90^c	19.31^ab	1.56^c	15.70^b	43.33^b	7.83^c	27.66^c
农田L5	18.36^a	59.42^ab	22.22^bc	1.08^d	37.30^c	60.15^c	9.38^c	56.72^a
撂荒地L6	18.24^a	57.51^ab	24.24^c	1.22^a	27.78^a	54.81^ac	9.45^c	50.41^a

指标	有机质	砂粒	粉粒	黏粒	容重	饱和含水量	初始含水量	总孔隙度	坡度	坡向
初始入渗率	0.737	-0.393	0.498	-0.279	-0.645	0.16	-0.620	0.651	0.480	0.480
稳定入渗率	0.813^*	-0.456	0.483	-0.083	-0.823^*	0.834^*	-0.242	0.860^*	-0.101	-0.101
平均入渗率	0.815^*	0.420	0.496	-0.206	-0.750	0.813^*	-0.581	0.773	0.266	0.266
60 min累积入渗量	0.834^*	-0.442	0.486	-0.125	-0.810^*	0.851^*	-0.440	0.845^*	0.038	0.038

指标	有机质	砂粒	粉粒	黏粒	容重	饱和含水量	初始含水量	总孔隙度	坡度	坡向
初始入渗率	0.737	-0.393	0.498	-0.279	-0.645	0.16	-0.620	0.651	0.480	0.480
稳定入渗率	0.813^*	-0.456	0.483	-0.083	-0.823^*	0.834^*	-0.242	0.860^*	-0.101	-0.101
平均入渗率	0.815^*	0.420	0.496	-0.206	-0.750	0.813^*	-0.581	0.773	0.266	0.266
60 min累积入渗量	0.834^*	-0.442	0.486	-0.125	-0.810^*	0.851^*	-0.440	0.845^*	0.038	0.038

指标	主成分
指标	1	2	3
方差贡献率/%	57.16	24.31	12.55
累积贡献率/%	57.16	81.47	94.02
特征值	5.8	2.4	1.3
有机质	0.891	0.331	-0.228
砂粒	-0.906	-0.238	-0.212
粉粒	0.948	-0.149	0.181
黏粒	-0.137	0.972	0.071
容重	0.980	-0.140	0.076
饱和含水量	0.968	0.048	-0.214
初始含水量	-0.009	0.467	0.873
总孔隙度	0.955	0.207	-0.121
坡度	0.444	-0.802	0.064
坡向	0.419	-0.611	0.537

Impacts of rapid land use change on soil infiltration in an arid desert area

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