Effects of Different Land Use Types on Soil Moisture in the Loess Region of Western Shanxi Province

SHI Zhengle; ZHANG Jianjun; SHEN Mingshuang; LIU Chang; HU Yawei; XU Qintao; LI Yang

doi:10.13870/j.cnki.stbcxb.2021.06.026

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Effects of Different Land Use Types on Soil Moisture in the Loess Region of Western Shanxi Province

更新时间：2025-03-12

- Effects of Different Land Use Types on Soil Moisture in the Loess Region of Western Shanxi Province
- Vol. 35, Issue 6, Pages: 190-197(2021)
- 作者机构：
  
  1. 北京林业大学水土保持学院,北京,100083
  2. 山西吉县森林生态系统国家野外科学观测研究站, 山西吉县,042200
  3. 水土保持国家林业局重点实验室(北京林业大学),北京,100083
  4. 林业生态工程教育部工程研究中心(北京林业大学),北京,100083
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2021.06.026
  CLC： S152.7
- Published：2021
- 稿件说明：
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SHI Zhengle, ZHANG Jianjun, SHEN Mingshuang, et al. Effects of Different Land Use Types on Soil Moisture in the Loess Region of Western Shanxi Province[J]. 2021, 35(6): 190-197.
DOI：

SHI Zhengle, ZHANG Jianjun, SHEN Mingshuang, et al. Effects of Different Land Use Types on Soil Moisture in the Loess Region of Western Shanxi Province[J]. 2021, 35(6): 190-197. DOI： 10.13870/j.cnki.stbcxb.2021.06.026.

摘要

为明确不同土地利用类型对土壤水分的影响，采用土钻法在2019年和2020年4—10月定期对晋西黄土区人工油松林地、荒草地、农地0—10 m土层的含水量进行了观测研究。结果表明：（1）人工油松林地0—10 m土层的蓄水量为1 281.13 mm，荒草地为1 712.85 mm，农地为1 804.77 mm。油松林地较荒草地和农地多消耗431.72，523.64 mm的水分，且多消耗的土壤水分主要来源于深层土壤。（2）3个土地利用类型0—10 m土层含水量的垂直变化可以划分为土壤水分剧烈变化层、弱变化层和稳定变化层，各层的含水量随时间的变化也不尽相同。（3）油松林根系的直接吸水深度为5.4 m，影响深度可达10 m土层以下，农作物的吸水深度为4.2 m，影响深度可达8 m土层以下。对研究区内地势平坦、交通便利的地方可种植农作物，促进当地农业经济建设；而针对油松林地土壤含水量低的现象，可采取适当水分管理措施降低林地耗水。

Abstract

Soil water content in artificial Pinus tabulaeformis forestland

native grassland and farmland in the loess region of western Shanxi province were observe and studied to define the effects of different land use types on soil moisture. The water content in 0—10 m soil layer was measured by soil core method from April to October in 2019 and 2020. The results showed that: (1) The soil water storage of the 0—10 m soil profile in artificial P. tabulaeformis forestland was 1 281.13 mm

1 712.85 mm in native grassland

and 1 804.77 mm in farmland. P. tabulaeformis forest land consumed 431.72 mm and 523.64 mm water more than wasteland and agricultural land

respectively

and the more consumed soil water mainly came from deep soil. (2) The vertical change of water content in 0—10 m soil layer of three land use types could be divided vertically into three layers

including severe-changing layer

weak changing layer and relatively stable layer

and the change of water content in each layer with time was also different. (3) The depth of root water absorption was 5.4 m for P. tabulaeformis

4.2 m for crops. The influence of depth was 10 m for P. tabulaeformis

8 m for crops. Crops could be planted on flat and accessible sites in the study area to promote the local agricultural economy. In view of the low soil water content in P. tabulaeformis forest land

appropriate water management measures could be used to reduce stand water depletion in P. tabulaeformis forestland.

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references

刘宥延, 刘兴元, 张博, 等.黄土高原丘陵区人工灌草生态系统水土保持功能评估[J].水土保持学报, 2020, 34(3):84-90, 97.

安文明, 韩晓阳, 李宗善, 等.黄土高原不同植被恢复方式对土壤水分坡面变化的影响[J].生态学报, 2018, 38(13):4852-4860.

何娜娜, 贾如浩, 叶苗泰, 等.黄土高原旱地苹果园油菜间作对土壤大孔隙结构的影响[J].水土保持学报, 2021, 35(1):259-264.

高思远, 张建军, 李梁, 等.黄土区水土保持林地的蓄水动态及雨水渗透深度[J].中国水土保持科学, 2019, 17(2):17-26.

Gou Q P, Zhu Q K. Response of deep soil moisture to different vegetation types in the Loess Plateau of northern Shannxi, China[J].Scientific Reports, 2021, 11(1):e15098.

Su B Q, Su Z X, Shangguan Z P. Trade-off analyses of plant biomass and soil moisture relations on the Loess Plateau[J].Catena, 2021, 197(1):e104946.

杨阳, 朱元骏, 安韶山.黄土高原生态水文过程研究进展[J].生态学报, 2018, 38(11):4052-4063.

程立平, 刘文兆, 李志.黄土塬区不同土地利用方式下深层土壤水分变化特征[J].生态学报, 2014, 34(8):1975-1983.

兰志龙, 潘小莲, 赵英, 等.黄土丘陵区不同土地利用模式对深层土壤含水量的影响[J].应用生态学报, 2017, 28(3):847-855.

雷斯越, 郭晋伟, 何亮, 等.黄土丘陵区退耕坡面草地恢复与土壤物理性质空间分异特征[J].水土保持学报, 2021, 35(1):251-258.

濮阳雪华, 王月玲, 赵志杰, 等.陕北黄土区不同植被恢复模式植被与土壤耦合关系研究[J].草业学报, 2021, 30(5):13-24.

王宪志, 赵西宁, 高晓东, 等.黄土高原苹果园土壤水分及水分生产力模拟[J].应用生态学报, 2021, 32(1):201-210.

黄艳丽, 李占斌, 苏辉, 等.人工林对黄土高原小流域上下游不同坡面土壤水分的影响[J].农业工程学报, 2018, 34(15):108-116.

赵荣玮, 张建军, 李玉婷, 等.晋西黄土区人工林地土壤水分特征及其对降雨的响应[J].水土保持学报, 2016, 30(1):178-183.

胡波, 陈丽华.黄土高原不同林地土壤水分特征及影响因子通径分析[J].中国水土保持科学, 2021, 19(1):79-86.

Li B B, Li P P, Zhang W T, et al. Deep soil moisture limits the sustainable vegetation restoration in arid and semi-arid Loess Plateau[J].Geoderma, 2021, 399:e115122.

Li B B, Zhang W T, Wang J, et al. Severe depletion of available deep soil water induced by revegetation on the arid and semiarid Loess Plateau[J].Forest Ecology and Management, 2021, 491:e119156.

Shen M S, Zhang J J, Zhang S H, et al. Seasonal variations in the influence of vegetation cover on soil water on the loess hillslope[J].Journal of Mountain Science, 2020, 17(9):2148-2160.

Li Y T, Yu Y, Sun R X, et al. Simulation of soil water dynamics in a black locust plantation on the Loess Plateau, Western Shanxi Province, China[J/OL].Water, 2021, 13(9):1213. DOI:10.3390/w13091213.

路远, 党廷辉, 成琦.黄土高原沟壑区苹果园土壤剖面水分及矿质氮分布特征[J].水土保持学报, 2021, 35(2):106-112, 121.

毛娜.典型黄土区不同坡向地形序列土壤碳与水分垂直分布特征及其影响因素[D].陕西杨凌:西北农林科技大学, 2018.

苟清平, 朱清科, 李依璇, 等.陕北黄土区不同林地土壤干燥化效应[J].生态学报, 2019, 39(19):7161-7168.

王舒, 马岚, 张栋, 等.晋西黄土区不同林龄人工刺槐林下植被及土壤水分特征[J].北京师范大学学报(自然科学版), 2016, 52(3):253-258.

张星星, 刘小芳, 赵勇钢, 等.黄土丘陵区柠条坡地水分空间异质性及其主控因素[J].中国水土保持科学, 2020, 18(6):24-32.

张建军, 李慧敏, 徐佳佳.黄土高原水土保持林对土壤水分的影响[J].生态学报, 2011, 31(23):71-81.

张敏, 刘爽, 刘勇, 等.黄土丘陵缓坡风沙区不同土地利用类型土壤水分变化特征[J].水土保持学报, 2019, 33(3):115-120, 128.

孔凌霄, 毕华兴, 周巧稚, 等.晋西黄土区不同立地刺槐林土壤水分动态特征[J].水土保持学报, 2018, 32(5):163-169.

王艳莉, 刘立超, 高艳红, 等.人工固沙植被区土壤水分动态及空间分布[J].中国沙漠, 2015, 35(4):942-950.

焦瑞, 赵英, 司炳成, 等.黄土高原退耕还林措施对深层土壤含水率的影响[J].干旱地区农业研究, 2017, 35(5):129-135.

朱炜歆, 牛俊杰, 刘庚, 等.植被类型对生长季黄土区土壤含水量的影响[J].干旱区资源与环境, 2016, 30(1):152-156.

邵明安, 贾小旭, 王云强, 等.黄土高原土壤干层研究进展与展望[J].地球科学进展, 2016, 31(1):14-22.

刘丙霞, 任健, 邵明安, 等.黄土高原北部人工灌草植被土壤干燥化过程研究[J].生态学报, 2020, 40(11):3795-3803.

Bolotov A G, Shein E V, Makarychev S V. Water retention capacity of soils in the Altai Region[J].Eurasian Soil Science, 2019, 52(2):187-192.

谭学进, 穆兴民, 高鹏, 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.

万艳萍, 赵洋毅, 段旭, 等.干湿交替对红河干旱河谷区土壤优先流形成特征的影响[J].应用生态学报, 2021, 32(7):2397-2406.

周宏.干旱区包气带土壤水分运移能量关系及驱动力研究评述[J].生态学报, 2019, 39(18):6586-6597.

Aa Y L, Wang G Q, Sun W C, et al. Stratification response of soil water content during rainfall events under different rainfall patterns[J].Hydrological Processes, 2018, 32(20):3128-3139.

Anooja T, Brijesh K Y, Jiří Š. Root water uptake under heterogeneous soil moisture conditions:An experimental study for unraveling compensatory root water uptake and hydraulic redistribution[J].Plant and Soil, 2020, 457:421-435.

Wang P, Song X F, Han D M, et al. A study of root water uptake of crops indicated by hydrogen and oxygen stable isotopes:A case in Shanxi Province, China[J].Agricultural Water Management, 2010, 97(3):475-482.

郭茹茹, 杨磊, 李宗善, 等.半干旱黄土高原苜蓿草地撂荒过程土壤水分变化特征[J].生态学报, 2020, 40(23):8618-8626.

郭利军, 王百田, 王旭虎.晋西黄土区不同土地利用的土壤水分灰关联分析[J].中国水土保持科学, 2020, 18(3):81-89.

柏勇, 杜静, 杨婷婷, 等.不同水土保持措施对石漠化区水土流失的影响[J].中国水土保持科学, 2018, 16(2):103-110.

赵丹阳, 毕华兴, 侯贵荣, 等.晋西黄土区典型林地土壤水分变化特征[J].水土保持学报, 2021, 35(1):181-187.

唐敏, 赵西宁, 高晓东, 等.黄土丘陵区不同土地利用类型土壤水分变化特征[J].应用生态学报, 2018, 29(3):765-774.

葛俸池, 许明祥.黄土丘陵沟壑区不同退耕模式的土壤水文性质影响对比[J].水土保持学报, 2021, 35(1):154-160, 168.

杜康, 张北赢, 李凯, 等.黄土丘陵区不同水体中氢氧同位素特征及相互关系[J].地球与环境, 2021, 49(3):270-276.

王宁, 毕华兴, 孔凌霄, 等.晋西黄土区不同密度刺槐林地土壤水分补偿特征[J].水土保持学报, 2019, 33(4):255-262.

周壮壮, 任宗萍, 李鹏, 等.不同植被覆盖下土壤含水量对降水的分级响应[J].中国水土保持科学, 2020, 18(6):62-71.

陈曦, 李志, 程立平, 等.黄土塬区大气降水的氢氧稳定同位素特征及水汽来源[J].生态学报, 2016, 36(1):98-106.

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