Spatial Differentiation Characteristics of Grassland Restoration and Soil Physical Properties of Slope in Hilly-gully Region of Loess Plateau

LEI Siyue; GUO Jinwei; HE Liang; HE Jie; XU Xiaoming; Lü Du; ZHANG Xiaoping

doi:10.13870/j.cnki.stbcxb.2021.01.036

您当前的位置：

首页 >

文章列表页 >

Spatial Differentiation Characteristics of Grassland Restoration and Soil Physical Properties of Slope in Hilly-gully Region of Loess Plateau

更新时间：2025-03-12

- Spatial Differentiation Characteristics of Grassland Restoration and Soil Physical Properties of Slope in Hilly-gully Region of Loess Plateau
- Vol. 35, Issue 1, Pages: 251-258(2021)
- 作者机构：
  
  西北农林科技大学水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点室, 陕西杨凌,712100
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2021.01.036
  CLC： S152.3
- Published：2021
- 稿件说明：
移动端阅览
LEI Siyue, GUO Jinwei, HE Liang, et al. Spatial Differentiation Characteristics of Grassland Restoration and Soil Physical Properties of Slope in Hilly-gully Region of Loess Plateau[J]. 2021, 35(1): 251-258.
DOI：

LEI Siyue, GUO Jinwei, HE Liang, et al. Spatial Differentiation Characteristics of Grassland Restoration and Soil Physical Properties of Slope in Hilly-gully Region of Loess Plateau[J]. 2021, 35(1): 251-258. DOI： 10.13870/j.cnki.stbcxb.2021.01.036.

摘要

为了解地形对草地恢复与土壤物理性质的影响以及草地恢复与土壤物理性质之间的影响机制，因地制宜为当地生态恢复提供科学依据。选择吴起县枣庄沟小流域为研究区，对退耕坡面不同坡位草地恢复与土壤物理性质分异特征进行研究。从峁顶到沟底设置8个采样位置，在4面坡共布设128个采样点进行植被调查和土样采集，将0—40 cm土壤分0—10，10—20，20—40 cm 3层进行土壤物理性质测定，并分析其与植被分布的相关关系。结果表明：不同坡位植被分布与土壤物理性质均表现出沟缘线以上的下坡位较优，沟缘线以下的陡沟坡较差的趋势；植被恢复对土壤团聚体有明显改善作用，但对其与土壤物理性质的改善主要集中在0—20 cm表层土壤，对20—40 cm土壤影响较弱；坡度对植被盖度与土壤容重、孔隙度和饱和持水量影响显著且具有极显著相关性，但对团聚体与颗粒组成无显著影响；植被恢复对土壤颗粒组成改善效果缓慢，若土壤颗粒组成被破坏，短期内很难恢复。

Abstract

In order to understand the effect of microtopography on vegetation restoration and soil physical properties

exploring the influence mechanism between grassland restoration and soil physical properties and to provide scientific basis for local ecological restoration. This study choose the Zaozhuanggou basin in Wuqi county as the study area

vegetation restoration and soil physical properties differentiation characteristics on the different landscape positions were studied. We chose 4 slopes and set eight sampling positions on every slope from top to bottom

a total of 128 sampling points of vegetation investigation and soil samples collected in this study. The soil was divided into three layers 0—10

10—20 and 20—40 cm for sampling and determining soil physical properties

analyzed the correlation between vegetation distribution and soil physical properties. The results showed that the vegetation distribution and soil physical properties on different landscape positions showed the tendency of lower slope better than others above the groove line

and the bottom slope is worst. The vegetation restoration has improvement effect on soil aggregate

the improvement of soil aggregate and soil physical properties caused by vegetation restoration was mainly concentrated on the surface soil of 0—20 cm

and weak in the soil of 20—40 cm. Gradient has a significant impact on vegetation coverage

soil bulk density

porocity and saturated water capacity. But it has no significant effect on the soil aggregate and soil particle composition. The effect of vegetation restoration on improving soil particle composition is slow. If the soil particle composition is destroyed

it will be difficult to recover in the short term.

关键词

Keywords

references

Yang X H, Zhang X P, Lv D, et al. Remote sensing estimation of the soil erosion cover-management factor for China's Loess Plateau[J].Land Degradation & Development,2020,31(15):1942-1955.

刘宝元,唐克丽,焦菊英,等. 黄河水沙时空图谱[M].2版.北京:科学出版社,2019:618-619.

Xu E Q, Zhang H Q. Change pathway and intersection of rainfall, soil, and land use influencing water-related soil erosion[J].Ecological Indicators, 2020,113:e106281.

Yang Y, Dou Y X, Liu D, et al. Spatial pattern and heterogeneity of soil moisture along a transect in a small catchment on the Loess Plateau[J].Journal of Hydrology,2017,550:466-477.

Ma H, Zhu Q K, Zhao W J. Soil water response to precipitation in different micro-topographies on the semi-arid Loess Plateau, China[J].Journal of Forestry Research,2020,31(1):245-256.

Bi H J, Zhang J J, Zhu J Z, et al. Spatial dynamics of soil moisture in a complex terrain in the semi-arid Loess Plateau Region, China[J]. Journal of the American Water Resources Association,2008,44(5):1121-1131.

王子婷,杨磊,李广,等. 半干旱黄土区苜蓿退化对坡面草本植物分布及多样性的影响[J].生态学报,2019,39(10):3720-3729.

Yu H Y, Zha T G, Zhang X X, et al. Spatial distribution of soil organic carbon may be predominantly regulated by topography in a small revegetated watershed[J].Catena,2020,188:e104459.

Liu Y, Zhang L P, Lu J K, et al. Topography affects the soil conditions and bacterial communities along a restoration gradient on Loess-Plateau[J].Applied Soil Ecology,2020,150(C):e103471.

闫瑞,张晓萍,闫胜军,等.1995-2014年北洛河流域植被恢复的地形分布特征[J].东北大学学报(自然科学版),2016,37(11):1598-1603.

赵文慧.黄土高原典型流域的植被特征及土壤养分响应的空间差异[D].陕西杨凌:西北农林科技大学, 2017.

闫瑞.黄土高原北洛河上游流域退耕还林草的水文响应模拟[D].陕西杨凌:西北农林科技大学,2017.

赵文慧,陈妮,闫瑞,等.近20年来北洛河流域植被覆盖度随地形因子变化特征探究[J].水土保持研究,2016,20(4):10-14.

王国梁,刘国彬,侯喜禄.黄土高原丘陵沟壑区植被恢复重建后的物种多样性研究[J].山地学报,2002,20(2):182-187.

赵成章,石福习,董小刚,等.祁连山北坡退化林地植被群落的自然恢复过程及土壤特征变化[J].生态学报,2011,31(1):115-122.

黄平,李廷轩,张佳宝,等.坡度和坡向对低山茶园土壤有机质空间变异的影响[J].土壤,2009,41(2):264-268.

朱志诚,贾东林,岳明.黄土高原中部草地群落初级生产[J].西北大学学报(自然科学版),1998,28(6):536-539.

Guillod B P, Orlowsky B, Miralles D G, et al. Reconciling spatial and temporal soil moisture effects on afternoon rainfall[J].Nature Communications,2015,6:DOI:10.1038/ncomms7443.

魏天兴,赵健,朱文德,等.退耕还林区水土保持植被恢复及物种多样性特征[J].西北林学院学报,2013,28(1):1-6.

Li Y Y, Shao M A. Change of soil physical properties under long-term natural vegetation restoration in the Loess Plateau of China[J].Journal of Arid Environments,2005,64(1):77-96.

Deng L, Wang K B, Tang Z S, et al. Soil organic carbon dynamics following natural vegetation restoration:Evidence from stable carbon isotopes (δ

C)[J].Agriculture Ecosystems and Environment,2016,221:235-244.

Deng L, Shangguan Z P, Sweeney S. Changes in soil carbon and nitrogen following land abandonment of farmland on the Loess Plateau, China[J].PLoS one,2013,8(8):e71923.

李裕元,邵明安,陈洪松,等.水蚀风蚀交错带植被恢复对土壤物理性质的影响[J].生态学报,2010,30(16):4306-4316.

Zhao D, Xu M X, Liu G B, et al. Effect of vegetation type on microstructure of soil aggregates on the Loess Plateau, China[J].Agriculture, Ecosystems & Environment,2017,242:1-8.

吕渡,杨亚辉,赵文慧,等.不同恢复类型植被细根分布及与土壤理化性质的耦合关系[J].生态学报,2018,38(11):3979-3987.

Dou Y X, Yang Y, An S S, et al. Effects of different vegetation restoration measures on soil aggregate stability and erodibility on the Loess Plateau, China[J].Catena,2020,185:e104294.

Views

1003

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Soil Moisture Retrieval Under Different Land Use Types in the Loess Area Using Electrical Resistivity Tomography

Impact of Soil Physical Crust Damage Caused by Grazing Trampling on Wind Erosion

Spatiotemporal Variation of Vegetation NEP on Loess Plateau and Its Responses to Temperature， Precipitation， and Grain-for-Green Program

Spatiotemporal Variation in Water Use Efficiency of Typical Ecosystems on the Loess Plateau Based on Biome-BGC Model

Accuracy of Composite Fingerprinting in Sediment Source Discrimination in Small Watersheds of the Loess Plateau

Related Author

ZHOU Shuyi

GAO Xiaodong

MA Nanfang

SHAO Xiaoya

ZHAO Xining

ZHAO Shirui

CHRISTOPHE Mupenzi

ZHANG Xiumei

Related Institution

State Key Laboratory of Soil and Water Conservation and Desertification Control， Northwest A&F University， Yangling

College of Water Resources and Architectural Engineering， Northwest A&F University， Yangling

College of Soil and Water Conservation Science and Engineering （Institute of Soil and Water Conservation），Northwest A&F University， Yangling

College of Soil and Water Conservation Science and Engineering （Institute of Soil and Water Conservation）， Northwest A&F University， State Key Laboratory of Soil and Water Conservation and Desertification Control，Northwest A&F University， Yangling

Faculty of Environmental Studies， University of Lay Adventists of Kigali， Kigali

⁰