太原师范学院 汾河流域科学发展研究中心,山西,太原,030012
纸质出版:2015
移动端阅览
刘庚, 牛俊杰, 朱炜歆, 等. 晋西北黄土丘陵区人工林地土壤水分亏缺评价[J]. 水土保持通报, 2015,35(5):309-314.
LIU Geng, NIU Junjie, ZHU Weixin, et al. Assessment on Soil Water Deficit Under Different Artificial Forestland in Loess Hilly Regions of Northwestern Shanxi Province[J]. Bulletin of Soiland Water Conservation, 2015, 35(5): 309-314.
刘庚, 牛俊杰, 朱炜歆, 等. 晋西北黄土丘陵区人工林地土壤水分亏缺评价[J]. 水土保持通报, 2015,35(5):309-314. DOI: 10.13961/j.cnki.stbctb.2015.05.057.
LIU Geng, NIU Junjie, ZHU Weixin, et al. Assessment on Soil Water Deficit Under Different Artificial Forestland in Loess Hilly Regions of Northwestern Shanxi Province[J]. Bulletin of Soiland Water Conservation, 2015, 35(5): 309-314. DOI: 10.13961/j.cnki.stbctb.2015.05.057.
[目的] 定量评价半干旱黄土丘陵区人工林地土壤水分亏缺现象
为科学指导该区域合理配置植被和生态恢复建设提供理论依据。[方法] 以地处晋西北的五寨县为目标研究区域
通过构建土壤水分亏缺定量评价模型
对柠条林(Caragana korshinskii)、小叶杨林(Populus simonii)、油松林(Pinus tabuliformis)土壤水分相对亏缺指数和样地土壤水分相对亏缺指数进行计算。[结果] 3种人工林地均有不同程度的土壤水分相对亏缺现象
小叶杨林和柠条林在0-200 cm有轻微土壤水分亏缺
小叶杨林在200-600 cm深度内没有土壤水分亏缺
柠条林在200 cm深度以下土壤水分亏缺值随土层深度增加而升高;油松林在0-200 cm土层深度内
土壤水分亏缺严重
在200 cm深度以下土壤水分亏缺值随土层深度增加而有所降低;3种林地的样地土壤水分相对亏缺指数分别为0.16
-0.12和0.31
油松林的土壤水分亏缺程度高于另外2种林地;3种人工林地均有不同程度的干层分布
以轻度和中度干层为主
油松林在浅层土壤有重度土壤干层发育。[结论] 晋西北黄土丘陵区3种人工林地中
油松林土壤水分亏缺最为严重。
[Objective] We aimed to quantitatively assess the soil water deficit under vegetation in the semiarid loess hilly region in order to provide theoretical support for the selection of vegetation types and ecological restoration pattern.[Methods] The compared soil water deficit index(CSWDI) and plot compared soil water deficit index(PCSWDI) of Caragana korshinskii
Populus simonii Carr and Pinus tabulaeformis in soil profiles of 0-600 cm deepth were calculated to quantify soil water deficit and its profile distribution under different vegetation types on April
May
June and July in Wuzhai County
Northwestern Shanxi Province.[Results] Soil water deficit appeared in all three artificial forestland. Soil water deficit was found in P. simonii and C. korshinskii in soil layers between 0 and 200 cm
however
it was hardly found in P. simonii between 200 and 600 cm. Below 200 cm
soil water deficit increased with increasing CSWDI in C. korshinskii. The P. tabulaeformis had led to a serious deep soil desiccation
especially in soil layers from 0 to 200 cm. Soil water deficit decreased in the layers below 200 cm with the increase of soil depths in P. tabulaeformis. PCSWDI of C. korshinskii
P. simonii and P. tabulaeformis was 0.16
-0.12 and 0.31
respectively. The soil water deficit of P. tabulaeformis was more severe than that in the others two forestland. The dried soil layer was distributed in all three artificial forestland with a different degree
mainly for mild and moderate dry layer distribution. Extreme dry layer presented in shallow soil of P. tabulaeformis.[Conclusion] The soil water deficit in the P. tabulaeformis was the severest among the three artificial forests in the loess hilly regions.
Legates D R, Mahmood R, Levia D, et al. Soil Moisture:A central and unifying theme in physical geography[J]. Progress in Physical Geography, 2011,35(1):65-86.
Chen Hongsong, Shao Ming'an, Li Yuyuan. Soil Desiccation in the Loess Plateau of China[J]. Geoderma, 2008,143(1):91-100.
费喜亮,张新民,景凌云,等.半干旱黄土区土壤水分垂直分布规律的研究:以甘肃省兰州市孙家岔流域为例[J].土壤学报,2013,50(4):652-656.
卫伟,温智,陈利顶,等.半干旱黄土丘陵区土壤结皮的地表水文效应[J].环境科学,2012,33(11):3901-3904.
Chen Liding, Wei Wei, Fu Bojie, et al. Soil and water conservation on the Loess Plateau in China:Review and perspective[J]. Progress in Physical Geography, 2007,31(4):389-403.
杨文治,余存祖.黄土高原区域治理与评价[M].北京:科学出版社,1992:45-49.
Wang Yunqiang, Shao Mingan, Shao Hongbo. A preliminary investigation of the dynamic characteristics of dried soil layers on the Loess Plateau of China[J]. Journal of Hydrology, 2010,381(1/2):9-17.
Liu Wenzhao, Zhang Xingchang, Dang Tinghui, et al. Soil water dynamics and deep soil recharge in a record wet year in the southern Loess Plateau of China[J]. Agriculture Water Management, 2010,97(8):1133-1138.
李洪建,王孟本,柴宝峰.黄土高原土壤水分变化的时空特征分析[J].应用生态学报,2003,14(4):515-519.
李正国,王仰麟,吴健生,等.基于TVDI的黄土高原地表干燥度与土地利用的关系研究[J].地理研究,2006,25(5):913-916.
段争虎,肖洪浪,宋耀选.黄土高原西部兰州市郊人工林地水分亏缺与调控研究[J].中国沙漠,2006,26(4):527-531.
肖列,薛萐,刘国彬.黄土丘陵区梯田果园土壤水分特征[J].植物营养与肥料学报,2013,19(4):964-971.
雷泽勇,刘心玲,周凯,等.辽西北沙地人工林植物水分亏缺与恢复研究[J].水土保持学报,2009,23(4):86-90.
王延平,邵明安,张兴昌.陕北黄土区陡坡地人工植被的土壤水分生态环境[J].生态学报,2008,28(8):3769-3778.
Rallo G, Provenzano G. Modelling eco-physiological response of table olive trees(
Olea europaea
L.)to soil water deficit conditions[J]. Agricultural Water Management, 2013(120):79-88.
Li Yan, Cohen Y, Wallach R, et al. On quantifying soil water deficit of a partially wetted root zone by the response of canopy or leaf conductance[J]. Agricultural Water Management, 2004,65(1):21-38.
Michelot A, Bréda N, Damesin C, et al. Differing growth responses to climatic variations and soil water deficits of
Fagus sylvatica, Quercus petraea
and
Pinus sylvestris
in a temperate forest[J]. Forest Ecology and Management, 2012,265(3):161-171.
Liang Zongsuo, Yang Jianwei, Shao Hongbo, et al. Investigation on water consumption characteristics and water use efficiency of poplar under soil water deficits on the Loess Platea[J]. Colloids and Surfaces B:Biointerfaces, 2006,53(1):23-28.
Mengistu D K. The influence of soil water deficit imposed during various developmental phases on physiological processes of tef(
Eragrostis tef
)[J]. Agriculture, Ecosystems & Environment, 2009,132(3/4):283-289.
孙中峰,张学培,张晓明,等.晋西黄土区林地坡面土壤水分异质性研究[J].干旱地区农业研究,2004,22(2):81-86.
贾志清.晋西北黄土丘陵沟壑区典型灌草植被土壤水分动态变化规律研究[J].水土保持通报,2006,26(1):10-15.
侯振宏,贺康宁,张小全.晋西黄土高原半干旱区刺槐林分需水量的研究[J].水土保持学报,2003,17(4):180-183.
段建军,王小利,张彩霞,等.黄土高原土壤干层评定指标的改进及分级标准[J].水土保持学报,2007,21(6):151-154.
李军,陈兵,李小芳,等.黄土高原不同干旱类型区苜蓿草地深层土壤干燥化效应[J].生态学报,2007,27(1):75-89.
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):3060-3068.
0
浏览量
1378
下载量
0
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621