Abstract:[Background] Windy and sandy region of North Shanxi where the severe water erosion and wind erosion happened is the most extremely frail eco-environment of Shanxi province. In the past few decades, large areas of plantations have been planted here for windbreaks and sand fixation. However, at the same time as it works, plantations can also absorb lots of water from soil and lead to soil desiccation. Jiajiayao catchment, located in Youyu County, is one of the most typical ecological fragile areas in windy and sandy region of North Shanxi province.[Methods] Due to soil moisture and grain size are the limiting factors for ecosystem restoration in this area, based on the field investigation, sampling and measurement, the characteristics of soil moisture and grain size of 6 different plantation types(11-year Pinus tabulaeformis, 21-year P. tabulaeformis, 23-year Larix principis-rupprechtii, 17-year P. tabulaeformis and Caragana korshinskii, C. korshinskii and Hippophae rhamnoides) in Jiajiayao catchment was analyzed in order to provide useful references for vegetation restoration.[Results] 1) There were considerably differences in characteristics of average soil moisture content in 0-100 cm soil profile among different plantation types. Mean soil moisture content of individual plantation type was about 4.62%-8.30%, and showed following sequence:Hippophae rhamnoides > 11-year P. tabulaeformis > C. korshinskii > 17-year P. tabulaeformis and C. korshinskii>23-year L. principis-rupprechtii > 21-year P. tabulaeformis. Mean soil moisture content in the topsoil (0-20 cm) among 6 plantation types was relatively low. Thereafter the pattern of variation began to be inconstant with the increase of depth. This may be explained by that the antecedent precipitation was in the uniform condition, while affected by plant transpiration, depth and density of root distribution, soil moisture content became complicated in deeper soil layers. 2) The grain size characteristic of all 6 plantation types was similar that silt and very fine sand content was the highest. However, silt content was the highest at C. korshinskii and H. rhamnoides, very fine sand content was the highest at the other plantation types. 3) The variation tendency of the grain size of different plantation types was not consistent in 0-100 cm soil profile. For the average grain size, the order was:23-year L. principis-rupprechtii > 11-year P. tabulaeformis > 21-year P. tabulaeformis > 17-year P. tabulaeformis and C. korshinskii > H. rhamnoides > C. korshinskii.[Conclusions] The water-holding capacity of H. rhamnoides and C. korshinskii was much better than the other plantation types. H. rhamnoides and C. korshinskii should be given priority in the process of vegetation restoration in windy and sandy region of North Shanxi. After years of vegetation restoration, the water consumption of plantations had increased in the study area. It was necessary to carry out the scientific management according to the soil water status, water consumption characteristics, and growth stages of plantations, such as adjusting the vegetation coverage and strengthening the protection of the undergrowth herb layer and litter layer.
郭伟1, 张鸾1, 刘爽1, 张凌云2. 晋北风沙区人工林土壤水分及粒度特征[J]. 中国水土保持科学, 2018, 16(2): 80-87.
GUO Wei, ZHANG Luan, LIU Shuang, ZHANG Lingyun. Characteristics of soil moisture and grain size in different plantation types in windy and sandy area of North Shanxi. SSWC, 2018, 16(2): 80-87.
王青杵,王改玲,石生新,等.晋北黄土丘陵区不同人工植被对水土流失和土壤水分含量的影响[J].水土保持学报,2012,26(2):71. WANG Qingchu, WANG Gailing, SHI Xinsheng, et al. Effect of different artificial vegetation on soil and water loss and soil moisture in Loess Hilly Area in Northern Shanxi Province[J]. Journal of Soil and Water Conservation,2012,26(2):71.
[2]
李耀林,郭忠升.平茬对半干旱黄土丘陵区柠条林地土壤水分的影响[J].生态学报,2011,31(10):2727. LI Yaolin, GUO Zhongsheng. Effects of cutting management on soil moisture in semi-arid Loess Hilly region[J]. Acta Ecologica Sinica,2011,31(10):2727.
[3]
莫保儒,蔡国军,杨磊,等.半干旱黄土区成熟柠条林地土壤水分利用及平衡特征[J].生态学报,2013,33(13):4011. MO Baoru, CAI Guojun, YANG Lei, et al. Soil water use and balance characteristics in mature forest land profile of Caragana korshinskii in semiarid loess area[J]. Acta Ecologica Sinica,2013,33(13):4011.
[4]
王力,卫三平,吴发启.黄土丘陵沟壑区农林草地土壤热量状况及植被生长响应:以燕沟流域为例[J].生态学报,2009,29(12):6578. WANG Li, WEI Sanping, WU Faqi. Soil heat and response of vegetation growth in the loess hilly and gully region:a case study of Yangou Catchment[J]. Acta Ecologica Sinica,2009,29(12):6578.
[5]
纪文婧,程小琴,韩海荣,等.山西太岳山好地方典型植被类型土壤理化特征.生态学杂志,2016,35(1):141. JI Wenjing, CHENG Xiaoqin, HAN Hairong, et al. Soil physicochemical properties of typical vegetation types in Haodifang, Taiyue Mountain of Shanxi[J]. Chinese Journal of Ecology,2016,35(1):141.
[6]
PAN Yanxia, WANG Xinping, JIA Rongliang, et al. Spatial variability of surface soil moisture contention in a revegetated desert area in Shapotou, Northern China[J]. Journal of Arid Environments,2008,72(9):1675.
[7]
SUR C Y, Jung Y, CHOL M H. Temporal stability and variability of field scale soil moisture on mountainous hillslopes in Northeast Asia[J]. Geoderma,2013,207/208:234.
[8]
符超峰,赵景波,卞子浩,等.毛乌素沙地中部不同类型沙丘土壤水分分布特征[J].地球科学与环境学报,2015,37(4):74. FU Chaofeng, ZHAO Jingbo, BIAN Zihao, et al. Distribution characteristics of soil moisture for different types of sand dunes in the center of Mu Us Sandy Land[J]. Journal of Earth Sciences and Environment,2015,37(4):74.
[9]
陈广庭.北京平原土壤机械组成和抗风蚀能力的分析[J].干早区资源与环境,1991,5(1):103. CHEN Guangting. Analysis of the composition of soil machinery and the corrosion resistance of the Beijing plain[J]. Journal of Arid Land Resources and Environment,1991,5(1):103.
[10]
杨磊,卫伟,莫保儒,等.半干旱黄土丘陵区不同人工植被恢复土壤水分的相对亏缺[J].生态学报,2011,31(11):3060. YANG Lei, WEI Wei, MO Baoru, et al. Soil water deficit under different artificial vegetation restoration in the semi-arid hilly region of the Loess Plateau[J]. Acta Ecologica Sinica,2011,31(11):3060.
[11]
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):7056. ZHANG Jianjun, LI Huimin, XU Jiajia. Soil moisture dynamics of water and soil conservation forest on the Loess Plateau[J]. Acta Ecologica Sinica,2011,31(23):7056.
[12]
高宇,樊军,彭小平,等.水蚀风蚀交错区典型植被土壤水分消耗和补充深度对比研究[J].生态学报,2014,34(23):7038. GAO Yu, FAN Jun, PENG Xiaoping, et al. Soil water depletion and infiltration under the typical vegetation in the water-wind erosion crisscross region[J]. Acta Ecologica Sinica,2014,34(23):7038.
[13]
LI Jun, CHEN Bing, LI Xiaofang, et al. Effects of deep soil desiccation on artificial forestlands in different vegetation zones on the Loess Plateau of China[J]. Acta Ecologica Sinica,2008,28(4):1429.
[14]
唐艳,刘连友,杨志鹏,等.毛乌素沙地南缘灌丛沙丘土壤水分与粒度特征研究[J].水土保持研究,2009,16(2):6. TANG Yan, LIU Lianyou, YANG Zhipeng, et al. Soil moisture and grain size characteristic of typical Nebkhas in south edge of Mu Us Sand land[J]. Research of Soil and Water Conservation,2009,16(2):6.
[15]
田丽慧,张登山,彭继平,等.高寒沙地人工植被恢复区地表沉积物粒度特征[J].中国沙漠,2015,35(1):32. TIAN Lihui, ZHANG Dengshan, PENG Jiping, et al. Grain size of land surface deposits in a vegetation restoration region of the alpine sandy land in Qinghai, China[J]. Journal of Desert Research,2015,35(1):32.
[16]
杨志勇,陈新闯,郭建英,等.乌兰布和沙漠不同土地利用类型粒度特征分析[J].中国水土保持,2015,7:50. YANG Zhiyong, CHEN Xinchuang, GUO Jianying, et al. Analysis of the characteristics of different land use types in Ulan Buh Desert[J]. Soil and Water Conservation In China,2015,7:50.
[17]
FOLK R L, WARD W C. Brazos river bar:A study in the significance of grain size parameters[J]. Journal of Sedimentary Research,1957,27(1):5.