[1]Liu Zhuoxin,Gao Peng,Mu Xingmin,et al.Effects of Vegetation Restoration on Soil Hydrophysical Properties in Loess Region[J].Research of Soil and Water Conservation,2023,30(06):206-213.[doi:10.13869/j.cnki.rswc.2023.06.046]
Copy
Effects of Vegetation Restoration on Soil Hydrophysical Properties in Loess Region
Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
30
Number of periods:
2023 06
Page number:
206-213
Column:
Public date:
2023-10-10
- Title:
- Effects of Vegetation Restoration on Soil Hydrophysical Properties in Loess Region
- CLC:
- S152
- DOI:
- 10.13869/j.cnki.rswc.2023.06.046
- Abstract:
- [Objective] Elucidating the influence of long-term returning farmland to forest, shrubland, and grassland on soil hydrophysical properties on the Loess Plateau is conducive to improving soil hydrology research and providing a theoretical basis for the subsequent ecological restoration of the Loess Plateau. [Methods] Through sampling analysis and double-ring infiltrometer test, the soil hydrophysical properties such as soil organic matter, bulk density, porosity, soil moisture and infiltration capacity of different vegetation restoration types were analyzed. [Results] Vegetation restoration had a significant impact on soil physical properties(p<0.05), and the resulting changes were most obvious in the 0—40 cm soil layer. The content of organic matter, porosity and the stability of water-stable aggregates significant increased, the soil bulk density decreased significantly. Converting farmland to forest, shrubland, and grassland enhanced soil infiltration capacity. Compared with farmland, the initial infiltration of Suide and Shenmu grassland increased by 50% and 31%, respectively; the stable infiltration rates of grassland, shrubs and forest in Suide area increased by 76%, 11% and 19%, respectively; those in Shenmu area increased by 53%, 128% and 58%, respectively. Soil stable infiltration and average infiltration were significantly negatively correlated with bulk density(p<0.05), and significantly positively correlated with total porosity, capillary porosity(p<0.05)and organic matter content(p<0.05). [Conclusion] Vegetation restoration has a significant effect on soil hydrophysical properties, soil infiltration performance has been significantly improved, and organic matter content, bulk density and porosity have significant effects on infiltration performance.
- References:
-
[1] 高鹏.黄河中游水沙变化及其对人类活动的响应[D].陕西杨凌:中国科学院研究生院(教育部水土保持与生态环境研究中心),2010.
Gao P. Streamflow and sediment discharge change trend and its response to human activities in the middle reaches of the Yellow River[D]. Yangling, Shaanxi: Graduate University of Chinese Academy of Sciences(Research Center for Soil and Water Conservation and Eco-Environment, Ministry of Education),2010.
[2] Mu X M, Zhang X Q, Shao H B, et al. Dynamic changes of sediment discharge and the influencing factors in the Yellow River, China, for the recent 90 years[J]. Clean-Soil, Air, Water, 2012,40(3):303-309.
[3] 李依璇,朱清,石若莹,等.2000—2018年黄土高原植被覆盖时空变化及影响因素[J].中国水土保持科学,2021,19(4):60-68.
Li Y X, Zhu Q, Shi R Y, et al. Spatial and temporal changes of vegetation cover and its influencing factors in the Loess Plateau from 2000 to 2018[J]. Science of Soil and Water Conservation, 2021,19(4):60-68.
[4] 穆兴民,顾朝军,赵广举,等.植被恢复对黄土高原产流模式变化影响初探[J].人民黄河,2019,41(10):30-39.
Mu X M, Gu C J, Zhao G J, et al. Preliminary assessment effect of vegetation restoration on runoff generation pattern of the Loess Plateau[J]. Yellow River, 2019,41(10):30-39.
[5] Ran Q H, Hong Y Y, Chen X X, et al. Impact of soil properties on water and sediment transport: A case study at a small catchment in the Loess Plateau[J]. Journal of Hydrology, 2019,574:211-215.
[6] 董莉丽.渭北旱塬植被恢复对土壤有机质和水稳性团聚体含量的影响[J].干旱区研究,2014,31(4):709-714.
Dong L L. Effects of Vegetation regeneration on soil organic matter content and water stable aggregates in the Weibei Dryland[J]. Arid Zone Research, 2014,31(4):709-714.
[7] 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.
Li Y Y, Shao M A, Chen H S, et al. Impacts of vegetation recovery on soil physical properties in the cross area of wind-water erosion[J]. Acta Ecologica Sinica, 2010,30(16):4306-4316.
[8] Cao C Y, Jiang D M, Teng X H, et al. Soil chemical and microbiological properties along a chronosequence of Caragana microphylla Lam. Plantations in the Horqin sandy land of Northeast China[J]. Applied Soil Ecology, 2008,40(1):78-85.
[9] 史德明,韦启潘,梁音,等.中国南方侵蚀土壤退化指标体系研究[J].水土保持学报,2000,14(3):1-9.
Shi D M, Wei Q P, Liang Y, et al. Study on degradation index system of eroded soils in southern China[J]. Journal of Soil and Water Conservation, 2000,14(3):1-9.
[10] Liu X, Zhang G C, Gary C, et al. Fractal features of soil particle-size distribution as affected by plant communities in the forested of Mountain Yimeng, China[J]. Geoderma, 2009,154(1/2):123-130.
[11] 焦梦妍,从怀军,姚静,等.自然恢复序列梯度上退耕地土壤容重变化及其蓄水性能效应[J].水土保持学报,2018,32(5):128-133.
Jiao M Y, Cong H J, Yao J, et al. Soil bulk density changes and its water-storage capacity of abandoned farmland in natural restoration series gradient of Loess Hilly-gully Region[J]. Journal of Soil and Water Conservation, 2018,32(5):128-133.
[12] 李同川.黄土高原土壤大孔隙特征及其对土壤水分的影响[D].陕西杨凌:西北农林科技大学,2017.
Li T C. Characteristics of soil macropore on the loess plateau and three effects on soil water[D]. Yangling, Shannxi: Northwest A & F University, 2017.
[13] 王梦军,张光灿,刘霞,等.沂蒙山林区不同森林群落土壤水分贮存与入渗特征[J].中国水土保持科学,2008,6(6):26-31.
Wang M J, Zhang G C, Liu X, et al. Characteristics of soil water infiltration and water-holding under different forest community in Yimeng Mountainous forest area[J]. Science of Soil and Water Conservation, 2008,6(6):26-31.
[14] 王国梁,刘国彬,周生路.黄土丘陵沟壑区小流域植被恢复对土壤稳定入渗的影响[J].自然资源学报,2003,18(5):529-535.
Wang G L, Liu G B, Zhou S L. The effect of vegetation restoration on soil stable infiltration rates in small watershed of loess gully region[J]. Journal of Natural Resources, 2003,18(5):529-535.
[15] 谭学进,高鹏,穆兴民,等.黄土区植被恢复对土壤物理性质的影响[J].中国环境科学,2019,39(2):713-722.
Tan X J, Gao P, Mu X M, et al. Effects of vegetation restoration on changes to soil physical properties on the loess plateau[J]. China Environmental Science, 2019,39(2):713-722.
[16] 陈文媛,张少妮,华瑞,等.黄土丘陵区林草恢复进程中土壤入渗特征研究[J].北京林业大学学报,2017,39(1):62-69.
Chen W Y, Zhang S N, Hua R, et al. Effects of forestland and grassland restoration process on soil infiltration characteristics in loess hilly region[J]. Journal of Beijing Forestry University, 2017,39(1):62-69.
[17] 刘畅,张建军,张海博,等.晋西黄土区退耕还林后土壤入渗特征及土壤质量评价[J].水土保持学报,2021,35(5):101-107.
Liu C, Zhang J J, Zhang H B, et al. Characteristics of soil infiltration and soil quality evaluation after conversion of farmland to forest in loess region of western Shanxi Province[J]. Journal of Soil and Water Conservation, 2021,35(5):101-107.
[18] 顾朝军.黄土区土壤水文物理特性及流域产汇流机制变化对植被恢复的响应[D].陕西杨凌:西北农林科技大学,2019.
Gu C J. Response of soil hydrological physical properties and changes of runoff yield and confluence to vegetation restoration in the loess region[D]. Yangling, Shannxi: Northwest A & F University, 2019.
[19] 查同刚.土壤理化分析[M].北京:中国林业出版社,2017.
Zha T G. Soil Physicochemical Analysis[M]. Beijing: China Forestry Publishing House, 2017.
[20] Tang B Z, Jiao J Y, Yan F C, et al. Variations in soil infiltration capacity after vegetation restoration in the hilly and gully regions of the Loess Plateau, China[J]. Journal of Soils and Sediments, 2019,19(3):1456-1466.
[21] Qiu D X, Xu R R, Wu C X, et al. Vegetation restoration improves soil hydrological properties by regulating soil physicochemical properties in the Loess Plateau, China[J]. Journal of Hydrology, 2022,609:1-12.
[22] Wang R, Dong Z B, Zhou Z T, et al. Effect of vegetation patchiness on the subsurface water distribution in abandoned farmland of the Loess Plateau, China[J]. Science of the Total Environment, 2020,746:1-15.
[23] 杨娥女,王宝荣,姚宏佳,等.黄土高原生物土壤结皮发育过程中颗粒态和矿物结合态有机碳变化特征[J].水土保持研究,2023,30(1):25-33,40.
Yang E N, Wang B R, Yao H J, et al. Dynamics of Particulate and Mineral-Associated Organic Carbon During the Development of Biological Soil Crusts in the Loess Plateau Province[J]. Research of Soil and Water Conservation, 2023,30(1):25-33,40.
[24] 常恩浩,李鹏,肖列,等.黄土丘陵沟壑区植被恢复演替过程中根系行为特征[J].生态学报,2017,39(6):2090-2100.
Chang E H, Li P, Xiao L, et al. The characteristics of root system behavior in vegetation succession in Loess Hilly and Gully Region Province[J]. Acta Ecologica Sinica, 2017,39(6):2090-2100.
[25] 赵明月,赵文武,刘源鑫.不同尺度下土壤粒径分布特征及其影响因子:以黄土丘陵沟壑区为例[J].生态学报,2015,35(14):4625-4632.
Zhao M Y, Zhao W W, Liu Y X. Comparative analysis of soil particle size distribution and its influence factors in different scales: a case study in the Loess Hilly-gully area Province[J]. Acta Ecologica Sinica, 2015,35(14):4625-4632.
[26] Belsky A J., Mwonga S M., Amundson R G., et al. Comparative effects of isolated trees on their undercanopy environments in high-and low-rainfall savannas[J]. Journal of Applied Ecology, 1993,30(1):143-155.
- Similar References:
Memo
-
Last Update:
2023-10-10