Soil Moisture Content under Artificial Robinnia pseudoacacia Forest at Different Slope Positions in the Zhonggou Minor Basin, Jingchuan County, Gansu Province

Expand
  • 1.College of Resources and Environmental Sciences, Gansu Agricultural University, Lanzhou 730070,Gansu,China;

    2. Guanshan Forest Farm in Jingchuan County, Pingliang 744306,Gansu,China;

    3.Guyuan Branch of Ningxia Academy of Agriculture and Forestry, Guyuan 756000, Ningxia,China

Received date: 2019-12-20

  Revised date: 2019-03-04

  Online published: 2019-09-11

Abstract

The soil hydrophysical properties under the artificial Robinia pseudoacacia forests in different landforms in a minor drainage basin in Jingchuan County, Gansu Province were measured using the “ring knife” method, and the soil moisture content was also measured using the oven drying method. The soil bulk density in 0-100 cm soil layer under the R. pseudoacacia plantations at different slope positions was in an order of the R. pseudoacacia forest on the hill top (1.24 g·cm3) > R. pseudoacacia forest at the gully bottom (1.20 g·cm3) > R. pseudoacacia forest (1.18 g·cm3) > R. pseudoacacia forest on the hill slope (1.16 g·cm3). The total soil porosity was in an order of the R. pseudoacacia forest on the hill slope (51.99%) > R. pseudoacacia forest in the gully (51.31%) > R. pseudoacacia forest at the tableland bottom (50.52%) > R. pseudoacacia forest at the tableland top (49.33%). The saturation moisture capacity and non-capillary moisture capacity of soil under the R. pseudoacacia forest on the hill slope were both the highest, then those under the R. pseudoacacia forests in gully and at the tableland bottom, and they were the lowest under the R. pseudoacacia forest on the hill top. The seasonal variation of soil moisture content under the forest was obvious, which could be divided into the soil moisture consumption period (from May to June), soil moisture supply period (July) and soil moisture reduction period (from August to September). The variable coefficient of soil moisture content under the forests in different landforms was increased at first and then decreased with the increase of soil depth, and it reached the highest value (Cv>0.3) in 40-80 cm soil layer. The results revealed that the soil moisture content was the highest under the R. pseudoacacia forest on the hill top, and then under the forests at the gully bottom and the on the gully tableland, and it was the lowest on the hill slope.

Cite this article

ZHANG Xiao-mei, DI Li, SHI Zai-jun, FEI Jun-e, WANG Zheng-an .

Soil Moisture Content under Artificial Robinnia pseudoacacia Forest at Different Slope Positions in the Zhonggou Minor Basin, Jingchuan County, Gansu Province[J]. Arid Zone Research, 2019 , 36(5) : 1300 -1308 . DOI: 10.13866/j.azr.2019.05.28

References

[1]Montzka C,Moradkhani H,Weihermuller L,et al.Hydraulic parameter estimation by remotelysensed top soil moisture observations with the particle filter[J].Journal of Hydrology,2011,399(34):410-421. [2]陈丽华,鲁绍伟,张学培,等.晋西黄土区主要造林树种林地土壤水分生态条件分析[J].水土保持研究,2008,15(1):79-86.[Chen Lihua,Lu Shaowei,Zhang Xuepei,et al.Analysis of soil water content of main afforestation species in western Shanxi of Loess Plateau[J].Research of Soil and Water Conservation,2008,15(1):79-86.] [3]常译方,毕华兴,高路博,等.晋西黄土区刺槐和油松林地土壤水分动态变化[J].中国水土保持科学,2014,12(4):21-27.[Chang Yifang,Bi Huaxing,Gao Lubo,et al.Dynamic changes of soil moisture in Robinia pseudoacacia and Pinus tabuliformis forestlands in loess region of Western Shanxi Province[J].Science of Soil and Water Conservation,2014,12(4):21-27.] [4]单长卷,墚宗锁,郝文芳.黄土高原刺槐林生长与土壤水分关系研究进展[J].西北植物学报,2003,23(8):1 341-1 346.[Shan Changjuan,Liang Zongsuo,Hao Wenfang.Review on growth of locust and soil water in Loess Plateau[J].Acta Botanica BorealiOccidentalia Sinica,2003,23(8):1 341-1 346.] [5]韩恩贤,韩刚.渭北高原沟壑区主要立地类型水热变化及对刺槐生长影响研究[J].干旱区资源与环境,2005,19(5):195-198.[Han Enxian,Han Gang.Effect of water and heat changes of main site types on the growth of Robinia pseudoacacia L.on Weibei Loess Plateau ravine region[J].Journal of Arid Land Resources and Environment,2005,19(5):195-198.] [6]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.[Huang Yanli,Li Zhanbin,Su Hui,et al.Effect of manmade forest on soil moisture of different slopes in upper and lower reaches of small watershed of Loess Plateau[J].Transactions of the CSAE,2018,34(15):108-116.] [7]董起广,张扬,陈田庆,等.黄土高原丘陵沟壑区小流域坡面土壤水分分布特征[J].中国农村水利水电,2018(7):65-73.[Dong Qiguang,Zhang Yang,Chen Tianqing,et al.Soil moisture distribution characteristics of small catchment slope in the Loess Plateau hillygully Region[J].China Rural Water and Hydropower,2018(7):65-73.] [8]韩芬,任烨,王彦辉,等.甘肃泾川刺槐林地穿透雨对降雨的响应[J].人民黄河,2015,37(7):90-94.[Han Fen,Ren Ye,Wang Yanhui,et al.Responses of throughfall to precipitation in black locust plantation at Jingchaun of Gansu[J].Yellow River,2015,37(7):90-94.] [9]甘淼,贾玉华,李同川,等.黄土区坡沟系统容重、饱和导水率和土壤含水量变化分析[J].干旱区研究,2018,35(2):315-324.[Gan Miao,Jia Yuhua,Li Tongchuan,et al.Variation of soil bulk density,saturated hydraulic conductivity and soil moisture content in a slopegully unit on the Northern Loess Plateau[J].Arid Zone Research,2018,35(2):315-324.] [10]何福红,黄明斌,党廷辉.黄土高原沟壑区小流域土壤水分空间分布特征[J].水土保持通报,2002,4(2):6-9.[He Fuhong,Huang Mingbin,Dang Tinghui.Soil water distribution characteristics in Wangdonggou watershed in gully region of Loess Plateau[J].Bulletin of Soil and Water Conservation,2002,4(2):6-9.] [11]景元书,范永强.低丘红壤不同坡位持水特性的比较[J].江西农业学报,2007,19(3 ):26-28.[Jing Yuanshu,Fan Yongqiang.Slope position difference of red soil water retention in low hilly area[J].Acta Agriculturae Jiangxi,2007,19(3):26-28.] [12]吕殿青,潘云.六道沟流域不同坡位不同土地利用方式下的土壤持水特征研究[J].中国农学通报,2008,24(8):279-282.[Lü Dianqing,Pan Yun.Study on soil retention characteristics of different position of slope of soil under different land uses in Liudaogou basin[J].Chinese Agricultural Science Bulletin,2008,24(8):279-282.] [13]中华人民共和国林业行业标准.森林土壤分析方法[M].北京:中国标准出版社,1999:1-108.[Forestry Industry Standard of the People’s Republic of China.Forest Soil Analysis Method[M].Beijing:China Standards Press,1999:1-108.] [14]王光玉.杉木混交林水源涵养和土壤性质研究[J].林业科学,2003,39(专刊1):15-20.[Wang Guangyu.Study on water conservation and soil properties of Chinese fir mixed stands[J].Scientia Silvae Sinicae,2003,39(Special Issue 1):15-20.] [15]马雪华.森林水文学[M].北京:中国林业出版社,1993:92-93.[Ma Xuehua.Forest Hydrology[M].Beijing:China Forestry Press,1993:92-93.]  [16]顾宇书,邢兆凯,韩友志,等.浑河上游4种典型水源林土壤物理性质及其水源涵养功能[J].东北林业大学学报,2013,41(1):37-41.[Gu Yushu,Xing Zhaokai,Han Youzhi,et al.Soil physical properties and water conservation function of four typical conservation forest in upper reaches of Hunhe River [J].Journal of Northeast Forestry University,2013,41(1):37-41.] [17]王忠诚,邓秀秀,崔卓卿,等.洞庭湖区主要森林类型土壤持水性能研究[J].中南林业科技大学学报,2016,36(5):79-84.[Wang Zhongcheng,Deng Xiuxiu,Cui Zhuoqing,et al.Research on water holding capacity of forest soil around Dongting Lake[J].Journal of Central South University of Forestry Science and Technology,2016,36(5):79-84.] [18]黄枝英,史宇,焦一之,等.北京山区典型人工林土壤水分动态研究[J].干旱区资源与环境,2012,26(11):166-171.[Huang Zhiying,Shi Yu,Jiao Yizhi,et al.Soil water dynamics of typical plantations in Beijing mountainous region[J].Journal of Arid Land Resources and Environment,2012,26(11):166-171.] [19]马骥,张维江.六盘山地区不同林地土壤水分动态变化特征初探[J].宁夏工程技术,2016,15(2):167-170.[Ma Ji,Zhang Weijiang.The dynamic change characteristics of soil water content in different forestland in Liupan Mountain area[J].Ningxia Engineering Technology,2016,15(2):167-170.] [20]王孟本,李洪建.晋西北黄土区人工林土壤水分动态的定量研究[J].生态学报,1995,15(2):178-184.[Wang Mengben,Li Hongjian.Quantitative study on the soil water dynamics of various forest plantations in the Loess Plateau region in Northwest Shanxi[J].Acta Ecologica Sinica,1995,15(2):178-184.]  [21]王正安,邸利,王彦辉,等.六盘山叠叠沟小流域 4 种植被土壤层水文调节功能的综合评价[J].干旱区资源与环境,2017,31(11):181-187.[Wang Zhengan,Di Li,Wang Yanhui,et al.Comprehensive evluation on the hydrological adjusting function of soils in four vegetation types in the small watershed of Diediegou,Liupan Mountains[J].Journal of Arid Land Resources and Environment,2017,31(11):181-187.] [22]鲁邵伟,毛富玲,靳芳,等.中国森林生态系统水源涵养功能[J].水土保持研究,2005,12(4):223-226.[Lu Shaowei,Mao Fuling,Jin Fang,et al.The water resource conservation of forest ecosystem in China[J].Research of Soil and Water Conservation,2005,12(4):223-226.] [23]孙中峰,张学培,刘卉芳,等.晋西黄土区坡面林地土壤持水性能研究[J].干旱区研究,2004,21(4):343-347.[Sun Zhongfeng,Zhang Xuepei,Liu Huifang,et al.Study on the waterconserving capabilities of soils under the sloped woodlands in the Loess area in West Shanxi Province[J].Arid Zone Research,2004,21(4):343-347.] [24]孔亮,蒙宽宏,陈宇,等.黑龙江省东部山地灌木林土壤水分动态变化[J].东北林业大学学报,2005,33(5):44-46.[Kong Liang,Meng Kuanhong,Chen Yu,et al.Soil water dynamic of several species of shrubs in east mountainous areas of Heilongjiang province[J].Journal of Northeast Forestry University,2005,33(5):44-46.] [25]陈洪松,邵明安,王克林.黄土区荒草地和裸地土壤水分的循环特征[J].应用生态学报,2005,16(10):1 853-1 857.[Chen Hongsong,Shao Mingan,Wang Kelin.Water cycling characteristics of grassland and bare land soils on Loess Plateau[J].Chinese Journal of Applied Ecology,2005,16(10):1 853-1 857.] [26]苏莹,陈林,李月飞,等.荒漠草原不同类型土壤水分时空变化特征[J].干旱区研究,2018,35(6):1 308-1 316.[Su Ying,Chen Lin,Li Yuefei,et al.Spatiotemporal variation of moisture content of different soil types in desert steppe[J].Arid Zone Research,2018,35(6):1 308-1 316.]
Outlines

/