干旱区生态环境知识资源中心(Arid): 黄土丘陵区小流域不同整地措施长期影响下的土壤水力学特性

Arid

	黄土丘陵区小流域不同整地措施长期影响下的土壤水力学特性
其他题名	Comparison of Soil Hydraulic Characteristics Under the Conditions of Longterm Land Preparation and Natural Slope in Longtan Catchment of the Loess Hilly Region
	冯天骄 1; 卫伟 1; 陈利顶 1; 陈蝶 1; 于洋 2; 杨磊 1
来源期刊	环境科学
ISSN	0250-3301
出版年	2017
卷号	38 期号:9 页码:3860-3870
中文摘要	水分是维持旱区生态系统健康与可持续性的关键因子. 整地措施能够重塑地表微地形,利于旱区雨水收集、侵蚀防控和促进植被恢复,整地长期影响下的土壤水力学性质是本文的研究重点. 以定西龙滩流域为研究区,通过野外采样与室内实验相结合,分析植被恢复过程中典型整地措施(鱼鳞坑、反坡台)的土壤水分时空分布、土壤水分特征曲线和水分常数,并辅以自然坡面为对照定量评价工程措施的土壤水力学特性. 结果表明: ① 整地可以有效提高土壤水分含量. 整地后土壤水分体积分数平均提高1.883%,相比自然坡面高出了22.62%. 反坡台和鱼鳞坑整地后,土壤水分含量分别提高了29.69% 和15.55%. ② 与对照相比,鱼鳞坑和反坡台的饱和含水量分别提高了7.52% 和4.24%,有效水含量分别提高了4.74% 和11.40%,整地措施能够提高土壤持水力和供水力,改善土壤水力学性质. ③ 整地措施对表层土壤持水能力和供水能力的影响较深层大,与对照相比,鱼鳞坑和反坡台表层土壤(0 ~ 20 cm)有效水分提高了38.75%和23.84%,而深层(60 ~ 80 cm)有效水分与自然坡面差异只有3.34%和3.85%; 土壤水分差异也随着土层深度而减少. 本研究定量评价了不同整地方式和自然坡面的土壤水分特性,其结果期望为脆弱生态系统植被恢复和水土资源管理提供科学依据.
英文摘要	Soil moisture plays a crucial role in maintaining the health and sustainability of dryland ecosystems. Terracing and other similar land preparations can reshape the natural slope and change underlying surface into different micro-landforms,which are significant for rainwater harvesting,erosion control,and vegetation promotion in arid regions. In this study,the Longtan Watershed in Dingxi region was selected as the study area. Based on in situ experiments,soil sampling analysis,and modeling simulation,the effects of land preparation and artificial vegetation (Fish-scale pit /Adverse grade tableland-Platycladus orientalis)on soil moisture characteristics curves and soil moisture constants were quantitatively analyzed. ①The land preparations could effectively improve the soil moisture content in the study catchment of Loess Plateau. Compared with natural slope,soil water content of land preparations increased by 1.883%(volume fraction)on average and fish-scale pit method and adverse grade tableland method enhanced the soil moisture by 29.69% and 15.55%,respectively. ② Compared with the natural slope,fish-scale pit and adverse grade tableland could significantly improve the soil hydraulic properties. After carrying out the land preparations,saturated soil water content and soil properties such as field capacity increased by 4.24%-11.40%,suggesting that land preparations can improve soil moisture and water supply ability. ③ Surface soil moisture characteristics were better than those of the underlying soil layers after land preparations. Compared with the natural slope,fish-scale pit and adverse grade tableland’s shallow soil layer (0-20 cm)increased the moisture by 38.75% and 23.84%,respectively,whereas in the deep layer (60-80 cm)the increment of moisture were only 3.34% and 3.85%, respectively. This research provides scientific basis for vegetation restoration and land improvement in fragile semi-arid ecosystems.
中文关键词	黄土高原 ; 整地方式 ; 土壤水分特征曲线 ; 土壤水力特性 ; 比水容量
英文关键词	Loess Plateau land preparation soil water characteristic curve soil hydraulic characteristics specific water capacity
语种	中文
国家	中国
收录类别	CSCD
WOS类目	ENVIRONMENTAL SCIENCES
WOS研究方向	Environmental Sciences & Ecology
CSCD记录号	CSCD:6063624
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/236188
作者单位	1.中国科学院生态环境研究中心, 城市与区域生态国家重点实验室, 北京 100085, 中国; 2.中国科学院生态环境研究中心, 城市与区域生态国家重点实验室;;水利部水土保持生态工程技术研究中心, 北京 100085, 中国
推荐引用方式 GB/T 7714	冯天骄,卫伟,陈利顶,等. 黄土丘陵区小流域不同整地措施长期影响下的土壤水力学特性[J],2017,38(9):3860-3870.
APA	冯天骄,卫伟,陈利顶,陈蝶,于洋,&杨磊.(2017).黄土丘陵区小流域不同整地措施长期影响下的土壤水力学特性.环境科学,38(9),3860-3870.
MLA	冯天骄,et al."黄土丘陵区小流域不同整地措施长期影响下的土壤水力学特性".环境科学 38.9(2017):3860-3870.