1. 桂林理工大学岩溶地区水污染控制与用水安全保障协同创新中心,广西,桂林,541004
2. 桂林理工大学广西环境污染控制理论与技术重点实验室科教结合科技创新基地,广西,桂林,541004
3. 中国电建集团华东勘测设计研究院有限公司,杭州,311100
4. 中国科学院环江喀斯特生态系统观测研究站, 广西 环江,547100
[ "郑金德(1998-),男,硕士研究生,主要从事水土保持与农业生态研究。E-mail:1601217135@qq.com" ]
纸质出版:2023
移动端阅览
郑金德, 潘焰菲, 徐勤学, 等. 桂西北喀斯特区石灰土与红壤坡地幼龄橘园降雨侵蚀特征[J]. 水土保持学报, 2023,37(6):11-17.
ZHENG Jinde, PAN Yanfei, XU Qinxue, et al. Rainfall Erosion Characteristics of Young Citrus Orchards on Calcareous Soil and Red Soil Slopes in Karst Areas of Northwest Guangxi[J]. 2023, 37(6): 11-17.
郑金德, 潘焰菲, 徐勤学, 等. 桂西北喀斯特区石灰土与红壤坡地幼龄橘园降雨侵蚀特征[J]. 水土保持学报, 2023,37(6):11-17. DOI: 10.13870/j.cnki.stbcxb.2023.06.002.
ZHENG Jinde, PAN Yanfei, XU Qinxue, et al. Rainfall Erosion Characteristics of Young Citrus Orchards on Calcareous Soil and Red Soil Slopes in Karst Areas of Northwest Guangxi[J]. 2023, 37(6): 11-17. DOI: 10.13870/j.cnki.stbcxb.2023.06.002.
为探究桂西北喀斯特区石灰土与红壤坡地幼龄橘园的降雨侵蚀特征
通过室内人工模拟降雨试验
研究3种降雨强度(30
60
90 mm/h)下
石灰土与红壤坡地幼龄橘园的产流产沙特征。结果表明:(1)降雨强度为30
60 mm/h时
红壤橘园的产流总量分别为石灰土橘园的2.46
1.83倍
且红壤橘园主要以地表产流为主
石灰土橘园主要以壤中流产流为主;当降雨强度为90 mm/h时
二者产流总量无显著性差异(p>0.05)
均以地表产流为主。(2)石灰土橘园与红壤橘园地表径流强度随降雨强度增大而增大;但随着降雨强度增大
石灰土橘园的壤中流径流强度呈先增大后减小趋势
红壤橘园壤中流径流强度却在减小。(3)降雨强度为60 mm/h时
红壤橘园产沙总量为石灰土橘园的3.74倍
当降雨强度为90 mm/h时
石灰土橘园产沙总量为红壤橘园的2.86倍;在降雨过程中
石灰土橘园产沙量随着降雨历时增大上下波动较为剧烈
红壤橘园产沙量随降雨历时增大波动幅度较小。(4)当降雨强度≥60 mm/h时
石灰土橘园与红壤橘园累积产沙量与累积产流量存在显著线性关系
且降雨强度越大线性关系越明显。研究结果可为喀斯特地区石灰土与红壤坡地幼龄橘园水土流失防治提供参考。
In order to investigate the characteristics of rainfall erosion of young citrus orchards on calcareous soil and red soil slopes in karst areas of northwestern Guangxi
an indoor artificial simulated rainfall experiment was conducted to study the runoff and sediment yield characteristics of young citrus orchards on calcareous soil and red soil slopes under three rainfall intensities (30
60
and 90 mm/h). The results showed that: (1) When the rainfall intensity was 30 and 60 mm/h
the total runoff yield of red soil citrus orchards was 2.46 and 1.83 times that of calcareous soil citrus orchards
respectively
and the red soil citrus orchards was dominated by surface runoff yield
while the calcareous soil citrus orchards was dominated by subsurface flow yield; when the rainfall intensity was 90 mm/h
there was no significant difference in the total amount of runoff between the two (p>0.05)
and both of them were mainly by surface runoff. (2) The surface runoff intensity of calcareous soil citrus orchards and red soil citrus orchards increased with the increase of rainfall intensity. However
with the increase of rainfall intensity
the subsurface flow intensity of calcareous soil citrus orchards showed a trend of first increasing and then decreasing
while the subsurface flow intensity of red soil citrus orchards was decreasing. (3) When the rainfall intensity was 60 mm/h
the total sediment yield of red soil citrus orange orchards was 3.74 times that of the calcareous soil citrus orchards
and when the rainfall intensity was 90 mm/h
the total sediment yield of the calcareous soil citrus orchards was 2.86 times that of red soil citrus orchards. During the rainfall process
the sediment yield of calcareous soil citrus orchards fluctuates sharply with the increase of rainfall duration
while the sediment yield of red soil citrus orchards was relatively small with the increase of rainfall duration. (4) When the rainfall intensity was more than 60 mm/h
there was a significant linear relationship between the cumulative sediment yield and cumulative runoff yield of calcareous soil and red soil orchards
and the greater the rainfall intensity
the more obvious the linear relationship was. The research results can provide reference and reasonable suggestions for the prevention and control of soil erosion in young citrus orchards on calcareous soil and red soil slopes in karst areas.
黄凯,刘瑞禄,覃莉,等.不同降雨条件下坡长对喀斯特坡面土壤侵蚀的影响[J].应用生态学报,2021,32(1):271-280.
马芊红,张科利.西南喀斯特地区土壤侵蚀研究进展与展望[J].地球科学进展,2018,33(11):1130-1141.
俞月凤,彭晚霞,宋同清,等.喀斯特峰丛洼地不同森林类型植物和土壤C、N、P化学计量特征[J]. 应用生态学报,2014,25(4):947-954.
饶珠阳,牙莉.2017年广西水果产业结构分析[J].广西农学报,2018,33(2):34-38.
涂安国,谢颂华,李英,等.红壤坡地柑桔园长期试验下水沙动态变化特征分析[J].水土保持学报,2018,32(2):160-165.
Cerdà A, Morera A G, Bodí M B. Soil and water losses from new citrus orchards growing on sloped soils in the western Mediterranean Basin[J].Earth Surface Processes and Landforms,2009,34(13):1822-1830.
孙永明,叶川,王学雄,等.赣南脐橙果园水土流失现状调查分析[J].水土保持研究,2014,21(2):67-71.
江才伦,彭良志,曹立,等.三峡库区紫色土坡地柑橘园不同耕作方式的水土流失研究[J].水土保持学报,2011,25(4):26-31,35.
Duan J, Liu Y J, Yang J, et al. Role of groundcover management in controlling soil erosion under extreme rainfall in citrus orchards of Southern China[J].Journal of Hydrology,2020,582:e124290.
刘勇,王玉杰,王红霞,等.长江三峡库区6种退耕还林模式涵养水源与保育土壤效益及其价值估算[J].中国水土保持科学,2014,12(6):50-58.
Gao Z C, Xu Q X, Si Q, et al. Effects of different straw mulch rates on the runoff and sediment yield of young citrus orchards with lime soil and red soil under simulated rainfall conditions in southwest China[J].Water,2022,14(7):e1119.
刘晓路,徐文玉,王可,等.红壤和紫色土坡面产流产沙特征对比[J].长江流域资源与环境,2022,31(8):1866-1872.
李杨,苏以荣,何寻阳,等.桂西北棕色石灰土和红壤有机碳矿化特征和差异[J].农业现代化研究,2012,33(5):632-635.
俞月凤,何铁光,宋同清,等.桂西北喀斯特地区石灰土养分空间变异特征[J].生态学报,2018,38(8):2906-2914.
陈洪松,冯腾,李成志,等.西南喀斯特地区土壤侵蚀特征研究现状与展望[J].水土保持学报,2018,32(1):10-16.
Fu Z Y, Chen H S, Zhang W, et al. Subsurface flow in a soil-mantled subtropical dolomite karst slope: A field rainfall simulation study[J].Geomorphology,2015,250:1-14.
常松涛,黄少燕,查轩,等.雨强和植被覆盖度对红壤坡面产流产沙的影响[J].水土保持学报,2019,33(3):58-63.
Fu Z Y, Chen H S, Xu Q X, et al. Role of epikarst in near-surface hydrological processes in a soil mantled subtropical dolomite karst slope: Implications of field rainfall simulation experiments[J].Hydrological Processes,2016,30(5):795-811.
Wang S, Fu Z Y, Chen H S, et al. Mechanisms of surface and subsurface runoff generation in subtropical soil-epikarst systems: Implications of rainfall simulation experiments on Karst slope[J].Journal of Hydrology,2020,580:e124370.
郭成久,孙景刚,苏芳莉,等.土壤容重对草甸土坡面养分流失特征的影响[J].水土保持学报,2012,26(6):27-30.
沈奕彤,郭成久,金珊,等.土壤容重对黑土坡面养分流失的影响[J].水土保持学报,2016,30(1):26-30.
吴秋菊,吴佳,王林华,等.黄土区坡耕地土壤结皮对入渗的影响[J].土壤学报,2015,52(2):303-311.
彭旭东,戴全厚,杨智,等.喀斯特山地石漠化过程中地表地下侵蚀产沙特征[J].土壤学报,2016,53(5):1237-1248.
李焱秋,戴全厚,甘艺贤,等.喀斯特裸坡地径流对降雨强度与坡度的响应[J].水土保持学报,2019,33(5):28-33.
钱婧,张丽萍,王文艳.红壤坡面土壤团聚体特性与侵蚀泥沙的相关性[J].生态学报,2018,38(5):1590-1599.
周梦玲,郭建斌,崔明,等.喀斯特坡地侵蚀泥沙养分流失与粒径分布的关系[J].水土保持学报,2019,33(6):54-60,71.
路培,王林华,吴发启.不同降雨强度下土壤结皮强度对侵蚀的影响[J].农业工程学报,2017,33(8):141-146.
田培,仇浩然,冯宇,等.雨强和坡度对红壤坡面产流产沙及侵蚀动力过程影响[J].水土保持研究,2020,27(6):1-8.
刘正堂,戴全厚,倪九派,等.喀斯特地区裸坡面土壤侵蚀的人工模拟降雨试验研究[J].水土保持学报,2013,27(5):12-16.
甘艺贤,戴全厚,伏文兵,等.基于模拟降雨试验的喀斯特坡耕地土壤侵蚀特征[J].应用生态学报,2016,27(9):2754-2760.
袁应飞,戴全厚,李昌兰,等.喀斯特典型坡耕地模拟降雨条件下的土壤侵蚀响应[J].水土保持学报,2016,30(3):24-28.
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