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三峡库区消落带农用坡地磷素径流流失特征
Phosphorus Loss from Sloping Cropland in Water Fluctuation Zone of the Three Gorges Reservoir

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刘莲 1,2   刘红兵 3   汪涛 1 *   朱波 1   姜世伟 1  
文摘 消落带是三峡库区重要的生态交错带,但自发农用和无序开发可能会造成更多的氮磷流失,进而加剧三峡库区水体富营养化。通过对库区连续3 a的定位监测( 2011 ~ 2013年),研究了三峡库区消落带农用坡地的磷素流失特征。结果表明:次降雨事件中常规施肥处理的地表径流、壤中流总磷平均浓度分别为0.848± 0.153、0.140±0.006 mg /L,其中地表径流中磷的形态以颗粒态为主,壤中流以溶解态的生物可利用磷为主。常规施肥下,地表径流、壤中流磷素年均流失通量分别为0.236±0.004、0.100±0.003 kg·hm~(-2),地表径流、壤中流磷素流失通量分别占总流失通量的70.2%、29.8%,地表径流是坡地磷素流失的主要途径,但壤中流也是不可忽视的重要途径。与常规施肥处理相比,减量施肥处理地表径流、壤中流磷素流失量分别降低了45.3%、40.0%。建议采取减量施肥的方式,以降低营养盐负荷,保护水环境。
其他语种文摘 Water fluctuation zone is an important riparian zone in the Three Gorges Reservoir area. Eutrophication could be exacerbated as the spontaneous and disorder reclamation of water fluctuation zone by local famers likely induce substantial soil phosphorus loss into receiving water bodies in the Three Gorges Reservoir. However,phosphorus loss characteristic via overland flow and interflow from sloping cropland in the water fluctuation zone of the Three Gorges Reservoir is unclear. In this study,plot experiments were conducted to study the characteristics of phosphorus loss via overland flow and interflow from sloping cropland in the water fluctuation zone of the Three Gorges Reservoir from 2011 to 2013. Results showed that the average concentration of total phosphorus in overland flow and interflow per runoff event were 0.848±0.153 mg /L and 0.140±0.006 mg /L in the conventional fertilization treatment,respectively. Particulate phosphorus was the main form in overland flow, while bioavailable phosphorus dominated in interflow. Annual phosphorus loss flux via overland flow for the conventional fertilization treatment was 0.236 ± 0.004 kg /hm~2,accounting for 70.2% of total hydrological phosphorus loss flux. By contrast,annual phosphorus loss flux via interflow for the conventional fertilization treatment was only 0.100 ± 0.003 kg /hm~2 that only accounted for 29.8% of total hydrological phosphorus loss flux. Our results indicated that overland flow was the main way of phosphorus loss from slope croplands in the water fluctuation zone of the Three Gorges Reservoir. However,phosphorus loss via interflow could not be ignored because its dominant form was bioavailable phosphorus. Moreover,compared with conventional fertilization,the optimized fertilization treatment reduced phosphorus losses of overland flow and interflow by 45.3% and 40.0%, respectively,which could represent an important practice of controlling phosphorus losses from sloping cropland in the water fluctuation zone of the Three Gorges Reservoir via reducing nitrogen fertilizer.
来源 长江流域资源与环境 ,2018,27(11):2609-2618 【核心库】
DOI 10.11870/cjlyzyyhj201811022
关键词 三峡库区 ; 消落带 ; 坡地 ; 磷素 ; 径流流失
地址

1. 中国科学院/水利部成都山地灾害与环境研究所, 四川, 成都, 610041  

2. 中国科学院大学, 北京, 100049  

3. 四川省农业厅土壤肥料与资源环境处, 四川, 成都, 610041

语种 中文
文献类型 研究性论文
ISSN 1004-8227
学科 农业基础科学;环境保护管理
基金 国家重点研发计划项目 ;  国家自然科学基金项目
文献收藏号 CSCD:6378312

参考文献 共 38 共2页

1.  Schindler D W. Eutrophication of lakes cannot be controlled by reducing nitrogen input: Results of a 37-year whole-ecosystem experiment. Produceedings of the National Academy of Science,2008,105(32):11254-11258 被引 169    
2.  颜晓. 长期施磷的产量效应及其环境风险评价. 环境科学,2013,34(8):3205-3210 被引 8    
3.  戚瑞生. 长期轮作与施肥对农田土壤磷素形态和吸持特性的影响. 土壤学报,2012,49(6):1136-1146 被引 32    
4.  Zheng Z M. Change in phosphorus fractions of a Humic Gleysol as influenced by cropping systems and nutrient sources. Canadian Journal of Soil Science,2001,81(2):175-183 被引 7    
5.  张广纳. 基于农业面源污染的三峡库区重庆段水质时空格局演变特征. 自然资源学报,2015,30(11):1872-1884 被引 8    
6.  姜世伟. 三峡库区消落带农用坡地氮素流失特征及其环境效应. 长江流域资源与环境,2017,26(8):1159-1168 被引 4    
7.  程瑞梅. 三峡库区典型消落带土壤化学性质变化. 林业科学,2017,53(2):19-25 被引 19    
8.  Bao Y H. Soil erosion in the riparian zone of the Three Gorges Reservoir,China. Hydrology Research,2015,46(2):212-221 被引 20    
9.  艾丽皎. 水体消落带国内外研究综述. 生态科学,2013,32(2):259-264 被引 27    
10.  程瑞梅. 消落带研究进展. 林业科学,2010,46(4):111-119 被引 43    
11.  刘晓. 基于RRM模型的三峡库区重庆开县消落区土地利用生态风险评价. 环境科学学报,2012,32(1):248-256 被引 31    
12.  刘丽琼. 三峡库区消落带土壤重金属分布特征及潜在风险评价. 中国环境科学,2011,31(7):1204-1211 被引 33    
13.  李楠. 北运河下游典型灌渠沉积物有机磷形态分布特征. 环境科学,2010,31(12):2911-2916 被引 15    
14.  胡刚. 三峡库区消落带下部区域土壤氮磷释放规律模拟实验研究. 长江流域资源与环境,2008,17(5):780-784 被引 19    
15.  马利民. 三峡库区消落区周期性干湿交替环境对土壤磷释放的影响. 环境科学,2008,29(4):1035-1039 被引 55    
16.  徐德星. 三峡入库河流大宁河回水区沉积物和消落带土壤磷形态及其分布特征研究. 环境科学,2009,30(5):1337-1344 被引 24    
17.  朱强. 三峡库区消落带土壤对磷的吸附和淹水下磷的形态变化. 土壤学报,2012,49(6):1128-1135 被引 18    
18.  Zhang B. Phosphorus fractions and phosphate sorption-release characteristics relevant to the soil composition of water-level-fluctuating zone of: Three Gorges Reservoir. Ecological Engineering,2012,40(3):153-159 被引 42    
19.  刘娜. 三峡库区消落带沉积物与土壤磷形态及分配特征研究. 水土保持学报,2016,30(4):261-267 被引 7    
20.  袁辉. 三峡库区消落带受淹土壤氮和磷释放的模拟实验. 环境科学研究,2008,21(1):103-106 被引 25    
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