[1]霍嘉仪,陈丽华*,及金楠,等.晋西黄土区不同林地类型对土壤水分特性的影响[J].山地学报,2018,(03):364-371.[doi:10.16089/j.cnki.1008-2786.000332]
 HUO Jiayi,CHEN Lihua*,JI Jinnan,et al.Effects of Different Types of Woodland on Soil Moisture Characteristics in the Loess Plateau of Western Shanxi Province, China[J].Mountain Research,2018,(03):364-371.[doi:10.16089/j.cnki.1008-2786.000332]
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晋西黄土区不同林地类型对土壤水分特性的影响()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2018年03期
页码:
364-371
栏目:
山地环境
出版日期:
2018-05-30

文章信息/Info

Title:
Effects of Different Types of Woodland on Soil Moisture Characteristics in the Loess Plateau of Western Shanxi Province, China
文章编号:
1008-2786-(2018)3-364-08
作者:
霍嘉仪1陈丽华12*及金楠1瞿文斌1
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
Author(s):
HUO Jiayi1 CHEN Lihua12* JI Jinnan1 QU Wenbin1
1.College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083,China; 2.National Field Research Station of Forest Ecosystem in Jixian County, Jixian, Shanxi 042200,China
关键词:
山西 黄土区 土壤含水量 土壤水分特征曲线 入渗速率
Keywords:
Shanxi province loess region soil moisture soil water characteristic curve infiltration rate
分类号:
S715.3
DOI:
10.16089/j.cnki.1008-2786.000332
文献标志码:
A
摘要:
为揭示晋西黄土区典型人工林土壤水分特征,本研究以刺槐林(Robinia pseudoacacia)、油松林(Pinus tabuliformis)、丁香林(Svzygium aromaticum)和裸地为研究对象,分析其土壤含水量、土壤水分特征曲线和土壤入渗速率。研究结果表明:(1)丁香林的土壤水分情况优于油松林地,刺槐林地的土壤水分状况最差,并且在80 cm处出现明显的土壤干层。(2)不同土层土壤水分特征曲线整体趋势均表现为快速下降-缓慢下降-基本平稳。丁香地土壤持水能力优于乔木林地,裸地土壤持水能力最差。(3)不同林分初始入渗速率、稳定入渗速率均表现为:丁香>刺槐>油松>裸地。Kostiakov、Philip和Horton模型对黄土区土壤水分入渗拟合效果均较好。综上,不同林分土壤水分特性差异较大,灌木林地的土壤水分特性要优于乔木林地,灌木林地更适合黄土区的自然条件,黄土区植被建设应该重视灌木种植,合理控制乔木林的种植范围。
Abstract:
To reveal the soil moisture characteristics of typical plantations in the loess region of western Shanxi Province, the soil moisture, water characteristic curve and infiltration rate were analyzed in the Robinia pseudoacacia, pinus tabuliformis, and Syzygium aromaticun plantations as well as the referenced bare land.The results indicated that(1)the soil moisture in the S.aromaticum plantation was higher than the P.tabuliformis plantation.Further, the soil moisture in the R.pseudoacacia plantation was the lowest with an obviously dry soil layer in 80 cm.(2)The soil water characteristic curve(SWCC)at different soil depths showed a trend of fast descending - slow descending - basically stable.Soil water-holding capacity in the S.aromaticum plantation was better than the arbor plantations, and the soil water holding capacity was the worst in the bare land.(3)The order of the initial and stable infiltration rates in different typical plantations were as follows: S.aromaticum, R.pseudoacacia, P.tabuliformis and the bare land.Kostiakov, Philip and Horton models fitted well with soil water infiltration in loess region.In short, the soil water characteristics were quite different among the typical plantations.The soil moisture characteristic in shrub plantation were better than arbor plantation, and shrub plantation was more suitable for the natural conditions of the loess region.Therefore, the shrub plantation should be paid more attention during vegetation construction, and the arbor plantation should be reasonably controlled in the loess region.

参考文献/References:

[1] 史小红,樊才睿,李畅游,等.呼伦贝尔草原不同放牧草场土壤水文特性研究[J].水土保持学报,2015,29(2):145-214 [SHI Xiaohong, FAN Cairui, LI Changyou, et al.Soil hydrological characteristics of different grazing system grassland in Hulun-Beier [J].Journal of Soil and Water Conservation, 2015, 29(2): 145-214]
[2] 王翠萍,廖超英,孙长忠,等.黄土地表生物结皮对土壤贮水性能及水分入渗特征的影响[J].干旱地区农业研究,2009,27(4):54-59 [WANG Cuiping, LIAO Chaoying, SUN Changzhong, et al.Effect of biological soil crusts on soil water storage capability and permeability in loess area [J].Agricultural Research in the Arid Areas, 2009, 27(4): 54-59]
[3] 李卓,刘永红,杨勤.土壤水分入渗影响机制研究综述[J].灌溉排水学报,2011,30(5):124-130 [LI Zhuo, LIU Yonghong, YANG Qin.Review on effects mechanism of soil water infiltration [J].Journal of Irrigation Drainage, 2011, 30(5): 124-130]
[4] 郭忠升,邵明安.半干旱区人工林地土壤入渗过程分析[J].土壤学报,2009,46(5):953-958 [GUO Zhongsheng, SHAO Mingan.Soil water infiltrating process in afforested land on slopes of the semiarid region of Loess Plateau [J].Acta Pedologica Sinica, 2009, 46(5): 953-958]
[5] 来剑斌,王全九.土壤水分特征曲线模型比较分析[J].水土保持学报,2003,17(1):137-140 [LAI Jianbin, WANG Quanjiu.Comparison of soil water retention curve model [J].Journal of Soil and Water Conservation, 2003, 17(1): 137-140]
[6] 孙迪,夏静芳,关德新,等.长白山阔叶红松林不同深度土壤水分特征曲线[J].应用生态学报,2010,21(6):1405-1409 [SUN Di, XIA Jingfang, GUAN Dexin, et al.Soil water characteristic curves at different soil depths in a broad-leaved Korean pine forest in Changbai Mountains.[J].Chinese Journal of Applied Ecology, 2010, 21(6):1405-1409]
[7] 杨文治.黄土高原土壤水资源与植树造林[J].自然资源学报,2011,16(5):433-438 [YANG Wenzhi.Soil water resources and afforestation in Loess Plateau [J].Journal of Natural Resources, 2011, 16(5): 433-438]
[8] 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 [SHAO Mingan, JIA Xiaoxu, WANG Yunqiang, et al.A review of studies on dried soil layers in the Loess Plateau [J].Advances in Earth Science, 2016, 31(1): 14-22]
[9] CHEN H, SHAO M, LI Y.Soil desiccation in the Loess Plateau of China [J].Geoderma, 2008, 143(1): 91-100
[10] FU B, WANG J, CHEN L, et al.The effect of land use on soil moisture variation in the Danangou catchment of the Loess Plateau, China [J].Catena, 2003, 54(1-2): 197-213
[11] CHEN L, HUANG Z, GONG J, et al.The effect of land cover/vegetation on soil water dynamic in the hilly area of the loess plateau, China [J].Catena, 2007, 70(2): 200-208
[12] 李民义,张建军,王春香,等.晋西黄土区不同土地利用方式对土壤物理性质的影响[J].水土保持学报,2013,27(3):125-131 [LI Minyi, ZHANG Jianjun, WANG Chunxiang, et al.Effects of land use types on soil physical properties in Loess Plateau of Western Shanxi [J].Journal of Soil and Water Conservation, 2013, 27(3): 125-131]
[13] 刘秀萍,陈丽华,陈吉虎.刺槐和油松根系密度分布特征研究[J].干旱区研究,2007,24(5):647-651 [LIU Xiuping, CHEN Lihua, CHEN Jihu.Study on the Distribution of root density of Robinia pseudoacacia L and Pinus tabulaeformis Carr [J].Arid Zone Research, 2007, 24(5): 647-651]
[14] 穆兴民,许学选,王文龙,等.黄土高原人工林对区域深层土壤水环境影响[J].土壤学报,2003,40(2):210-217 [MU Xingmin, XU Xuexuan, WANG Wenlong, et al.Impact of artificial forest on soil moisture of the deep soil layer on loess plateau [J].Acta Pedologica Sinica, 2003, 40(2): 210-217]
[15] 常译方,毕华兴,许华森,等.晋西黄土区不同密度刺槐林对土壤水分的影响[J].水土保持学报,2015,29(6):227-232 [CHANG Yifang, BI Huaxing, XU Huasen, et al.Influence of different densities of Robinia pseudoacacia forest on soil moisture in Loess Region of Western Shanxi Province [J].Journal of Soil and Water Conservation, 2015, 29(6): 227-232]
[16] 牛俊杰,赵景波,王尚义.汾河流域上游人工林地深层土壤干燥化探讨[J].地理研究,2007,26(4):773-781 [NIU Junjie, ZHAO Jingbo, WANG Shangyi.A study on plantation soil desiccation in the upper reaches of the Fenhe River basin based on deep soil experiments [J].Geographical Research, 2007, 26(4): 773-781]
[17] 王力,邵明安,王全九.林地土壤水分运动研究述评[J].林业科学,2005,41(2):147-153 [WANG Li, SHAO Mingan, WANG Quanjiu.Review on soil water movement in forestland [J].Scientia Silvae Sinicae, 2005, 41(2): 147-153]
[18] 王志强,刘宝元,张岩.不同植被类型对厚层黄土剖面水分含量的影响[J].地理学报,2008,63(7):703-713 [WANG Zhiqiang, LIU Baoyuan, ZHANG Yan.Effects of different vegetation types on soil moisture in deep loess soil profiles [J].Acta Geographica Sinica, 2008, 63(7): 703-713]
[19] 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):7056-7066 [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): 7056-7066]
[20] CHEN L, WANG J, WEI W, et al.Effects of landscape restoration on soil water storage and water use in the Loess Plateau Region, China [J].Forest Ecology & Management, 2010, 259(7): 1291-1298
[21] BATES JD, SVEJCAR TS, MILLER RF.Litter decomposition in cut and uncut western juniper woodlands [J].Journal of Arid Environments, 2007, 70(2): 222-236
[22] 李红,范素芳,张光灿,等.黄土丘陵区退耕还林后不同林地土壤孔隙与贮水特性[J].水土保持通报,2010,30(1):27-30 [LI Hong, FAN Sufang, ZHANG Guangcan, et al.Characteristics of soil water-holding and soil porosity under different tree species after conversion of cropland to forest in the loess hilly region [J].Bulletin of Soil and Water Conservation, 2010, 30(1): 27-30]
[23] 刘彩虹,卞建民,王宇.吉林西部盐碱土壤水力学参数特征及其影响因素[J].东北大学学报,2016,37(2):268-272 [LIU Caihong, BIAN Jianmin, WANG Yu.Characteristics of soil hydraulic parameters and impact factor analysis for saline-alkali soils in the western Jilin Province [J].Journal of Northeastern University(Natural Science), 2016, 37(2): 268-272]
[24] 郑荣伟,冯绍元,郑艳侠.北京通州区典型农田土壤水分特征曲线测定及影响因素分析[J].灌溉排水学报,2011,30(3):77-81 [ZHENG Rongwei, FENG Shaoyuan, ZHENG Yanxia.Discussion on the soil water characteristic curve of the agricultural soil in the new city of Tongzhou [J].Journal of Irrigation and Drainage, 2011, 30(3): 77-81]
[25] 吕殿青,王宏,王玲.离心机法测定持水特征中的土壤收缩变化研究[J].水土保持学报,2010,24(3):209-216 [LV Dianqing, WANG Hong, WANG Ling.Soil shrinking change during measuring retention characteristics by centrifugal method [J].Journal of Soil and Water Conservation, 2010, 24(3): 209-216]
[26] 宁婷,郭忠升,李耀林.黄土丘陵区撂荒坡地土壤水分特征曲线及水分常数的垂直变异[J].水土保持学报,2014,28(3):166-170 [NING Ting, GUO Zhongsheng, LI Yaolin.Soil water characteristic curves and soil water constants at different depths in the abandoned sloping field of loess hilly region [J].Journal of Soil and Water Conservation, 2014, 28(3): 166-170]
[27] 邢旭光,赵文刚,马孝义,等.土壤水分特征曲线测定过程中土壤收缩特性研究[J].水利学报,2015,46(10):1181-1188 [XING Xuguang, ZHAO Wengang, MA Xiaoyi, et al.Study on soil shrinkage characteristics during soil water characteristic curve measurement [J].Journal of Hydraulic Engineering, 2015, 46(10): 1181-1188]
[28] 席彩云,余新晓,徐娟,等.北京密云山区典型林地土壤入渗特征[J].北京林业大学学报,2009,31(5):42-47 [XI Caiyun, YU Xinxiao, XU Juan, et al.Soil Infiltration Characteristics of Typical Plantations in Mountainous Area of Miyun,Beijing [J].Journal of Beijing Forestry University, 2009, 31(5): 42-47]
[29] 党宏忠,周泽福,赵雨森,等.祁连山水源涵养林土壤水文特征研究[J].林业科学研究,2006,19(1):39-44 [DANG Hongzhong, ZHOU Zefu, ZHAO Yusen, et al.Soil hydrological characteristics of water conservation forest in Qilian mountains [J].Forest Research, 2006, 19(1): 39-44]
[30] 高婵婵,赵传燕,王超,等.黑河上游天老池流域不同植被下土壤理化性质和入渗特征[J].水土保持学报,2016,30(1):117-126 [GAO Chanchan, ZHAO Chuanyan, WANG Chao, et al.Soil physicochemical properties and infiltration characteristics under different vegetation types in Tianlaochi watershed in the upstream of Heihe River [J].Journal of Soil and Water Conservation, 2016, 30(1): 117-126]
[31] MEI X, ZHU Q, MA L, et al.Effect of stand origin and slope position on infiltration pattern and preferential flow on a Loess hillslope [J].Land Degradation & Development, 2018: 1-13
[32] WANG S, FU BJ, GAO GY, et al.The hydrological responses of different land cover types in a re-vegetation catchment area of the Loess Plateau [J].Hydrology and Earth System Sciences Discussions, 2012, 9(5): 5809-5835
[33] 金建新,桂林国,尹志荣,等.宁夏典型土壤持水性能及收缩特征[J].水土保持研究,2017,24(4):279-283 [JIN Jianguo, GUI Linguo, YIN Zhirong, et al.Soil moisture curve and shrinkage characteristic of different areas in Ningxia [J].Research of Soil and Water Conservation, 2017, 24(4): 279-283]

相似文献/References:

[1]上官铁梁,张峰.云顶山植被及其垂直分布研究[J].山地学报,1991,(01):19.
[2]张峰.山西关帝山野生植物资源研究[J].山地学报,1994,(03):181.
[3]李卓玉,张峰,李学风.山西关帝山药用植物资源研究[J].山地学报,1994,(03):187.
[4]郑凤英,张金屯,张峰,等.山西省草地资源及合理利用[J].山地学报,1996,(01):33.
[5]柴宝峰,李毳.山西太岳山种子植物区系特征[J].山地学报,1997,(03):162.
[6]茹文明.山西中条山东部野生植物资源[J].山地学报,1999,(04):386.
[7]武俊智,上官铁梁,张婕,等.旅游干扰对马仑亚高山草甸植物物种多样性的影响[J].山地学报,2007,(05):534.

备注/Memo

备注/Memo:
收稿日期(Received date):2017-12-25; 改回日期(Accepted date): 2018-05-29
基金项目(Foundation item):国家重点研发计划项目(2016YFC0501704)。[National Key Research and Development Program of China(2016YFC0501704)]
作者简介(Biography):霍嘉仪(1994-),女,山西吕梁人,硕士研究生,主要从事林业生态工程方面的研究。[HUO Jiayi(1994-), female, born in Luliang, Shanxi Province, M.Sc.candidate, research on forestry ecological engineering ] E-mail:490560679@qq.com
*通讯作者(Corresponding author):陈丽华(1957-),女,博士,教授,主要从事林业生态工程方面的研究。[CHEN Lihua(1957-), female, Ph.D., professor, research on forestry ecological engineering] E-mail:c-lihua@bjfu.edu.cn
更新日期/Last Update: 2018-05-30