1. 北京林业大学水土保持学院,北京,100083
2. 国家林业局水土保持与荒漠化防治重点实验室,北京,100083
[ "朱方方(1993-),女,硕士研究生,主要从事土壤侵蚀研究。E-mail:Fangf0506@163.com" ]
纸质出版:2020
移动端阅览
朱方方, 程金花, 郑雪慧, 等. 马尾松林地不同枯落物覆盖下土壤入渗特征[J]. 水土保持学报, 2020,34(4):85-90.
ZHU Fangfang, CHENG Jinhua, ZHENG Xuehui, et al. Soil Infiltration Characteristics Under Different Litter Covers in[J]. 2020, 34(4): 85-90.
朱方方, 程金花, 郑雪慧, 等. 马尾松林地不同枯落物覆盖下土壤入渗特征[J]. 水土保持学报, 2020,34(4):85-90. DOI: 10.13870/j.cnki.stbcxb.2020.04.013.
ZHU Fangfang, CHENG Jinhua, ZHENG Xuehui, et al. Soil Infiltration Characteristics Under Different Litter Covers in[J]. 2020, 34(4): 85-90. DOI: 10.13870/j.cnki.stbcxb.2020.04.013.
采用室内人工降雨模拟试验,在径流小区尺度上观测坡面产流过程,并用WatchDog1400土壤水分自动监测站观测土壤体积含水率变化过程,研究枯落物覆盖下坡面水分入渗特征。结果表明:(1)土壤入渗滞后时间随着枯落物覆盖量的增加而增大,在坡度上体现为10°>5°;(2)土壤入渗率随雨强、枯落物覆盖量增加而增大,随坡度增大而减小;土壤储水量随覆盖量增加先增大后减小,在雨强方面体现为120 mm/h>60 mm/h;(3)逐步回归结果表明,土壤入渗滞后时间、入渗率和储水量与枯落物覆盖量呈线性关系,滞后时间、入渗率与枯落物覆盖量呈一次函数正相关关系,储水量与覆盖量呈二次函数关系。研究结果可为低效林枯落物水源涵养功能研究提供依据。
Using laboratory artificial simulation rainfall experiment
the runoff process was observed on the scale of runoff plot
and the change process of soil volume moisture content was observed with Watchdog 1400 soil moisture automatic monitoring station to study the water infiltration characteristics of the slope under litter cover. The results were as follows:(1) The lag time of soil infiltration increases with the increase of litter coverage
and the slope was 10°>5°; (2) The infiltration rate of soil increases with the increase of rainfall intensity and litter coverage
and decreases with the increase of slope; the soil water storage first increases and then decreases with the increase of coverage
and the rainfall intensity is 120 mm/h>60 mm/h; (3) Stepwise regression shows that the soil infiltration lag time
infiltration rate and water storage capacity are linearly related to the amount of litter coverage
the lag time
infiltration rate and litter coverage are positively correlated with each other
the water storage and coverage has a quadratic function. The results can provide a basis for the research on the water source conservation function of the low-efficiency forest litter of Pinus massoniana.
黄俊,金平伟,李敏,等.径流小区尺度土壤入渗率影响因子与估算模型研究[J].农业机械学报,2016,47(8):171-178.
Sato Y, Kumagai T, Kume A, et al. Experimental analysis of moisture dynamics of litter layers-the effects of rainfall conditions and leaf shapes[J].Hydrological Processes,2004,18(16):3007-3018.
陈佩岩,马岚,梅雪梅,等.降雨过程中不同密度枯落物对各土层含水率动态影响[J].北京林业大学学报,2018,40(11):93-101.
侯贵荣,余新晓,刘自强,等.不同降雨强度下北京山区典型林地土壤水分时空变化特征[J].水土保持学报,2017,31(3):209-215.
邹小阳,牛文全,许健,等.残膜对土壤水分入渗的影响及入渗模型适用性分析[J].灌溉排水学报,2016,35(9):1-7,12.
王东旺,吕廷波,何新林,等.不同覆膜宽度对棉花土壤水分及地温的影响研究[J].节水灌溉,2018(12):33-37,43.
王红兰,唐翔宇,张维,等.施用生物炭对紫色土坡耕地耕层土壤水力学性质的影响[J].农业工程学报,2015,31(4):107-112.
魏永霞,王鹤,刘慧,等.生物炭对黑土区土壤水分及其入渗性能的影响[J].农业机械学报,2019,50(9):290-299.
陈胜男,胡钧铭,徐宪立,等.绿肥压青粉垄保护性耕作对土壤水分入渗及其后延效应的影响[J].中国农业气象,2018,39(12):778-785.
于庆峰,苗庆丰,史海滨,等.耕作方式对秸秆覆盖玉米田春播期土壤水热盐状况的影响[J].水土保持研究,2019,26(3):265-268.
张金珠,王振华,虎胆·吐马尔白.具有秸秆夹层层状土壤一维垂直入渗水盐分布特征[J].土壤,2014,46(5):954-960.
韩胜强,王振华,李文昊,等.不同可降解膜覆盖对一维土柱土壤水分入渗和蒸发的影响[J].中国农村水利水电,2019(8):42-46.
何子淼,肖培青,郝仕龙,等.黄丘区野外草被坡面土壤入渗参数变化规律与模拟研究[J].水土保持学报,2018,32(2):74-79.
张敬晓.黄土丘陵区林地干化土壤水分入渗及迁移规律研究[D].陕西杨凌:西北农林科技大学,2017.
舒维花,蒋齐,王占军,等.宁夏盐池沙地不同密度人工柠条林土壤水分时空变化分析[J].干旱区资源与环境,2012,26(12):172-176.
曹云生,赵艳玲.不同灌木林分枯落物层与土壤层水源涵养能力研究[J].水土保持研究,2019,26(6):179-183.
阿茹·苏里坦,常顺利,张毓涛.天山林区不同群落土壤水分入渗特性的对比分析与模拟[J].生态学报,2019,39(24):9111-9118.
倪含斌,张丽萍.神东矿区堆积弃土坡地入渗规律试验研究[J].水土保持学报,2007,21(3):28-31.
薛建辉,郝奇林,何常清,等.岷江上游两种亚高山林分枯落物层水文特征研究[J].水土保持学报,2009,23(3):168-172.
李波,李晔,韩惟怡,等.人工降雨条件下不同粒径泥沙中氮磷流失特征分析[J].水土保持学报,2016,30(3):39-43.
李兆松,王兵,汪建芳,等.铁杆蒿与白羊草枯落物覆盖量对黄土坡面流水动力特性的影响[J].农业工程学报,2018,34(17):151-157.
刘绪军,任宪平,杨亚娟,等.东北黑土区植物篱土壤入渗性能研究[J].水土保持通报,2017,37(2):45-49.
付玉娟,祝陈梦媛,张旭东,等.农田下垫面处理对降雨入渗的影响[J].水土保持研究,2019,26(4):74-79.
孙佳美,余新晓,李瀚之,等.模拟降雨下枯落物调控坡面产流产沙过程及特征研究[J].水利学报,2017,48(3):341-350.
喻阳华,李光容,严令斌,等.赤水河上游主要树种枯落物调蓄水分效应[J].中国水土保持科学,2015,13(3):39-44.
0
浏览量
1051
下载量
3
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621