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紫色砂岩区不同植被类型土壤优先流特征及其影响因素
引用本文:陈晓冰,;张洪江,;李世友,;张福明,;程金花,;魏虎伟,;田香姣.紫色砂岩区不同植被类型土壤优先流特征及其影响因素[J].中国水土保持科学,2014(6):42-49.
作者姓名:陈晓冰  ;张洪江  ;李世友  ;张福明  ;程金花  ;魏虎伟  ;田香姣
作者单位:[1]北京林业大学水土保持学院,北京100083; [2]重庆市江津区四面山森林资源管理局,重庆402296
基金项目:国家林业局推广项目“三峡库区低山丘陵区水土保持型植物群落建设技术”([2012]42); “十二五”农村领域国家科技计划课题“农田水土保持生物防护关键技术研究”(2011BAD31B02); 国家自然科学基金“长江三峡库区紫色砂岩林地坡面优先路径及其机理研究”(41271300),“三峡库区优先流影响土壤养分流失机制研究”(30900866)
摘    要:以三峡库区内的重庆市四面山针阔混交林、竹林和草地3种不同植被类型土地为研究对象,应用亮蓝染色示踪法和图像分析法,同时结合SPSS软件对比研究紫色砂岩区针阔混交林、竹林和草地3种不同植被类型下的土壤优先流特征及其影响因素。结果表明:1)3种植被类型下土壤优先流的主要发生区域不同,竹林和草地的土壤优先流主要发生在0~20 cm土壤表层,而针阔混交林的土壤优先流主要发生在10~40 cm土层;2)针阔混交林的土壤优先路径数量较竹林和草地多,优先路径发育程度表现为针阔混交林〉竹林〉草地;3)根系直径d影响土壤中优先流的发生,

关 键 词:针阔混交林  竹林  草地  优先路径  根系径级  土壤质地  土壤水力特性参数

Characteristics and influencing factors of preferential flow in different vegetation types of purple sandstone regions
Institution:Chen Xiaobing, Zhang Hongjiang,Li Shiyou,Zhang Fuming,Cheng Jinhua,Wei Huwei,Tian Xiangjiao (1. College of Soil and Water Conservation, Beijing Forestry University, 100083, Beijing, China; 2. Forest Resources Authority in Simian Mountain of Jiangjin District of Chongqing City, 402296, Chongqing, China)
Abstract:This paper focused on the forestland with three different vegetation types,i. e.,conifer +broadleaf forestland,Phyllostachys pubescens forestland and grassland in purple sandstone regions of the Simianshan Mountain in the Three Gorges Reservoir Area of Chongqing,using the methods of brilliant blue dye,image analysis and the SPSS software to present the soil preferential flow features and the influencing factors of the three vegetation types. The research results showed that: 1) The soil preferential flow zones were different for the three vegetation types,the soil preferential flow occurred in0- 20 cm of soil surface layer of the Phyllostachys pubescens forestland and grassland,while it always occurred in the 10- 40 cm of soil layer in the conifer + broadleaf forestland. 2) The conifer + broadleaf forestland had more soil preferential flow paths than in the Phyllostachys pubescens forestland andgrassland,the development degree of the soil preferential flow was in the order of conifer + broadleaf forestland Phyllostachys pubescens forest land grassland. 3) The root system impacted the occurrence of soil preferential flow: the root diameter between 3 and 5 mm had a noticeable impact on the soil preferential flow of conifer + broadleaf forestland; however,the soil preferential flow of the Phyllostachys pubescens forestland and grassland were affected mainly by the root diameter between 1 and 3 mm. 4) The mass fraction of the sand in the three different vegetation types affected the occurrence of the soil preferential flow,in the meantime,the soil preferential flow had an impact on the saturated soil hydraulic conductivity: it contributed to raise the saturated soil hydraulic conductivity.
Keywords:conifer + broadleaf forestland  Phyllostachys pubescens forestland  grassland  preferential flow path  root diameter  soil texture  soil hydraulic characteristic parameters
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