The Long-term Variations and Influencing Factors of Soil Saturated Hydraulic Conductivity in Terraces on the Loess Plateau
Author:
Clc Number:

S152.7

  • Article
  • | |
  • Metrics
  • |
  • Reference [32]
  • |
  • Related [20]
  • | | |
  • Comments
    Abstract:

    [Objective] The long-term variations of soil saturated hydraulic conductivity (Ks) and its primary controlling factors in terraces on the Loess Plateau were explored. [Methods] Terraces were selected for three land use types, i.e. farmland, orchard, and grassland, with slope designated as the control. Soil samples were collected from slopes and terraces with construction ages of 7, 20, 30 and 40 years to determine the Ks and soil physicochemical properties. The Kruskal-Wallis H test, Spearman correlation analysis, and partial least squares path model (PLS-PM) were conducted to examine the impact of terrace construction on Ks and its temporal variations, as well as the influencing factors. [Results] (1) The Ks of terraces under different land use types exhibited varying patterns with increasing ages of terrace construction. The Ks of farmland increased continuously with construction age of 7, 20, 30 and 40 years, increasing from 0.18 mm/min to 0.28 mm/min, with a growth rate of 55.56%. The Ks of orchard increased with the increase of construction years firstly, then showed a decreasing trend after 30 years, and the Ks of orchard with a construction age of 30 years was significantly higher than that of orchard with a construction age of 7 years, increasing from 0.12 mm/min to 0.35 mm/min, with a growth rate of 191.67%. The Ks of grassland increased with the increase of construction years firstly, then remained relatively stable after 20 years, and the Ks of grassland with a construction age of 20 years was significantly higher than that of grassland with a construction age of 7 years, increasing from 0.14 mm/min to 0.31 mm/min, with a growth rate of 121.43%. (2) The primary factors influencing Ks included soil particle size distribution, soil bulk density, and mean weight diameter of aggregates, with the path coefficients being -0.431, -0.561 and 0.226, respectively. [Conclusion] The variation in the impact of terrace land use types on soil properties resulted in varying patterns of Ks with increasing ages of terrace construction. The results can provide a basis for the subsequent management of terraces and the development of efficient dryland farming.

    Reference
    [1] TAN M L, GASSMAN P W, YANG X Y, et al. A review of SWAT applications, performance and future needs for simulation of hydro-climatic extremes[J].Advances in Water Resources,2020,143:e103662.
    [2] 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,2019,574:211-225.
    [3] BEVEN K J, KIRKBY M J, FREER J E, et al. A history of TOPMODEL[J].Hydrology and Earth System Sciences,2021,25(2):527-549.
    [4] RAN Q H, CHEN X X, HONG Y Y, et al. Impacts of terracing on hydrological processes: A case study from the Loess Plateau of China[J].Journal of Hydrology,2020,588:e125045.
    [5] ARNÁEZ J, LANA-RENAULT N, LASANTA T, et al. Effects of farming terraces on hydrological and geomorphological processes. A review[J].Catena,2015,128:122-134.
    [6] LU Y H, LI X B, XIN L J, et al. Mapping the terraces on the Loess Plateau based on a deep learning-based model at 1.89 m resolution[J].Scientific Data,2023,10(1):e115.
    [7] TIAN P, TIAN X J, GENG R, et al. Response of soil erosion to vegetation restoration and terracing on the Loess Plateau[J].Catena,2023,227:e107103.
    [8] 新华社.中共中央办公厅国务院办公厅印发《关于加强新时代水土保持工作的意见》[Z].中华人民共和国国务院公报,2023(2):5-8. Xinhua News Agency. The General Office of the Central Committee of the CPC and the General Office of the State Council Print and Issue the Opinions on Strengthening Water and Soil Conservation in the New Era[Z].Gazette of the State Council of the People’s Republic of China,2023(2):5-8.
    [9] 新华社.中共中央国务院印发《黄河流域生态保护和高质量发展规划纲要》[Z].中华人民共和国国务院公报,2021(30):15-35. Xinhua News Agency. The Central Committee of the CPC and the State Council Print and Issue the Outlines for the Plan for Ecological Protection and High-quality Development of the Yellow River Basin[Z].Gazette of the State Council of the People’s Republic of China,2021(30):15-35.
    [10] 中华人民共和国国家发展和改革委员会.黄土高原地区综合治理规划大纲(2010-2030年)[Z].2010:39. National Development and Reform Commission People’s Republic of China. Outline of the Comprehensive Management Plan for the Loess Plateau (2010-2030)[Z].2010:39.
    [11] 董世杰,辛良杰,李升发,等.中国梯田撂荒程度及空间格局分异研究[J].地理学报,2023,78(1):3-15. DONG S J, XIN L J, LI S F, et al. The extent and spatial distribution of terrace abandonment in China[J].Acta Geographica Sinica,2023,78(1):3-15.
    [12] 李宗善,杨磊,王国梁,等.黄土高原水土流失治理现状、问题及对策[J].生态学报,2019,39(20):7398-7409. LI Z S, YANG L, WANG G L, et al. The management of soil and water conservation in the Loess Plateau of China: Present situations, problems, and counter-solutions[J].Acta Ecologica Sinica,2019,39(20):7398-7409.
    [13] 薛萐,刘国彬,张超,等.黄土高原丘陵区坡改梯后的土壤质量效应[J].农业工程学报,2011,27(4):310-316. XUE S, LIU G B, ZHANG C, et al. Effects of terracing slope cropland on soil quality in Hilly Region of Loess Plateau[J].Transactions of the Chinese Society of Agricultural Engineering,2011,27(4):310-316.
    [14] ZHAO W, WANG M H, CHEN C B, et al. Variations, controls and predictions of soil saturated hydraulic conductivity under different land use types in the alpine region of Tibet, China[J].Geoderma Regional,2023,35:e00723.
    [15] WU X T, YANG Y, HE T, et al. Temporal variability of saturated hydraulic conductivity on a typical black soil slope of Northeast China[J].Catena,2024,236:e107742.
    [16] HE L, DUAN X Q, DING S W, et al. Construction and evaluation of pedotransfer functions for saturated hydraulic conductivity in the granite red soil regions of Southern China[J].Journal of Hydrology: Regional Studies,2023,50:e101539.
    [17] 杨震,黄萱,佘冬立.晋西北黄土丘陵区土壤饱和导水率的空间分布特征及影响因素[J].水土保持学报,2020,34(6):178-184. YANG Z, HUANG X, SHE D L. Spatial distribution characteristics and influencing factors of soil saturated hydraulic conductivity in the Loess Hilly Region of northwestern Shanxi[J].Journal of Soil and Water Conservation,2020,34(6):178-184.
    [18] LIU S Z, WANG Y Q, AN Z S, et al. Watershed spatial heterogeneity of soil saturated hydraulic conductivity as affected by landscape unit in the critical zone[J].Catena,2021,203:e105322.
    [19] 毛娜,黄来明,邵明安.黄土区坡面尺度不同植被类型土壤饱和导水率剖面分布及影响因素[J].土壤,2019,51(2):381-389. MAO N, HUANG L M, SHAO M A. Profile distribution of soil saturated hydraulic conductivity and controlling factors under different vegetations on slope in loess region[J].Soils,2019,51(2):381-389.
    [20] 赵春雷,邵明安,贾小旭.黄土高原北部坡面尺度土壤饱和导水率分布与模拟[J].水科学进展,2014,25(6):806-815. ZHAO C L, SHAO M A, JIA X X. Distribution and simulation of saturated soil hydraulic conductivity at a slope of northern Loess Plateau[J].Advances in Water Science,2014,25(6):806-815.
    [21] 王紫薇,邵明安,黄来明,等.青海省东部不同土地利用方式下土壤饱和导水率分布及其影响因素[J].水土保持学报,2021,35(3):150-155. WANG Z W, SHAO M A, HUANG L M, et al. Distribution and influencing factors of soil saturated hydraulic conductivity under different land use patterns in eastern Qinghai Province[J].Journal of Soil and Water Conservation,2021,35(3):150-155.
    [22] ZHU P Z, ZHANG G H, ZHANG B J. Soil saturated hydraulic conductivity of typical revegetated plants on steep gully slopes of Chinese Loess Plateau[J].Geoderma,2022,412:e115717.
    [23] 张益,林毅雁,贾国栋,等.北京山区典型植被类型土壤饱和导水率及其影响因素[J].水土保持学报,2022,36(6):171-178. ZHANG Y, LIN Y Y, JIA G D, et al. Soil saturated hydraulic conductivity and its influencing factors of typical vegetation types in Beijing mountainous area[J].Journal of Soil and Water Conservation,2022,36(6):171-178.
    [24] 鲍士旦.土壤农化分析[M].3版.北京: 中国农业出版社,2000:20-34. BAO S D. Soil and Agricultural Chemistry Analysis[M].3rd ed. Beijing: China Agriculture Press,2000:20-34.
    [25] 中华人民共和国国家林业局.LY/T 1215—1999,森林土壤水分—物理性质的测定[S].北京: 标准出版社,1999:22-24. State Forestry Administration of the People’s Republic of China. LY/T 1215—1999, Determination of forest soil water-physical properties[S].Beijing:Standards Press,1999:22-24.
    [26] 徐远慧,冯璐,屈媛媛,等.黄土丘陵沟壑区退耕还草年限对土壤性质和入渗性能的影响[J].水土保持学报,2022,36(2):57-63. XU Y H, FENG L, QU Y Y, et al. Effects of different restoration years of Grain for Green on soil properties and infiltration performance in loess Gully Region[J]. Journal of Soil and Water Conservation,2022,36(2):57-63.
    [27] ZHU P Z, ZHANG G H, WANG C S, et al. Variation in soil infiltration properties under different land use/cover in the black soil region of Northeast China[J].International Soil and Water Conservation Research,2024,12(2):379-387.
    [28] HAO H X, WEI Y J, CAO D N, et al. Vegetation restoration and fine roots promote soil infiltrability in heavy-textured soils[J].Soil and Tillage Research,2020,198:e104542.
    [29] QIAN X, GU J, SUN W, et al. Changes in the soil nutrient levels, enzyme activities, microbial community function, and structure during apple orchard maturation[J].Applied Soil Ecology,2014,77:18-25.
    [30] WANG Y Q, SHAO M A, LIU Z P, et al. Regional-scale variation and distribution patterns of soil saturated hydraulic conductivities in surface and subsurface layers in the Loessial soils of China[J].Journal of Hydrology,2013,487:13-23.
    [31] 李中恺,李小雁,周沙,等.土壤—植被—水文耦合过程与机制研究进展[J].中国科学:地球科学,2022,52(11):2105-2138. LI Z K, LI X Y, ZHOU S, et al. A comprehensive review on coupled processes and mechanisms of soil—vegetation—hydrology, and recent research advances[J].Scientia Sinica (Terrae),2022,52(11):2105-2138.
    [32] 王子龙,赵勇钢,赵世伟,等.退耕典型草地土壤饱和导水率及其影响因素研究[J].草地学报,2016,24(6):1254-1262. WANG Z L, ZHAO Y G, ZHAO S W, et al. Study on soil saturated hydraulic conductivity and its influencing factors in typical grassland of farmland conversion[J].Acta Agrestia Sinica,2016,24(6):1254-1262.
    Cited by
    Comments
    Comments
    分享到微博
    Submit
Get Citation
Share
Article Metrics
  • Abstract:54
  • PDF: 215
  • HTML: 281
  • Cited by: 0
History
  • Received:June 14,2024
  • Revised:July 11,2024
  • Online: January 17,2025
Article QR Code