武汉理工大学 资源与环境工程学院,湖北,武汉,430070
纸质出版:2016
移动端阅览
赵绍林, 李晔, 赵培培, 等. 三峡库区不同坡度石灰土坡耕地磷素流失特征[J]. 水土保持通报, 2016,36(6):115-120.
ZHAO Shaolin, LI Ye, ZHAO Peipei, et al. Characteristics of Phosphorus Loss in Sloping Farmland of Limestone Soil Under Different Gradients in Three Gorges Reservoir Area[J]. Bulletin of Soiland Water Conservation, 2016, 36(6): 115-120.
赵绍林, 李晔, 赵培培, 等. 三峡库区不同坡度石灰土坡耕地磷素流失特征[J]. 水土保持通报, 2016,36(6):115-120. DOI: 10.13961/j.cnki.stbctb.2016.06.019.
ZHAO Shaolin, LI Ye, ZHAO Peipei, et al. Characteristics of Phosphorus Loss in Sloping Farmland of Limestone Soil Under Different Gradients in Three Gorges Reservoir Area[J]. Bulletin of Soiland Water Conservation, 2016, 36(6): 115-120. DOI: 10.13961/j.cnki.stbctb.2016.06.019.
[目的] 研究石灰土坡耕地在不同坡度下的磷素流失规律,以期为三峡库区农业面源污染的防治和水资源保护提供基础数据。[方法] 在三峡库区香溪河流域坡耕地修建径流小区进行原位人工降雨试验,在雨强1.5 mm/min时,分析10°,15°和20°这3种坡度下坡耕地的径流量、泥沙浓度,以及地表径流中总磷、颗粒态磷,泥沙中总磷、速效磷浓度的变化趋势,并对径流泥沙进行无机磷分级试验。[结果] 坡度越大,地表径流量、径流总量、泥沙流失量越大,初始产流时间越短,但坡度对径流中泥沙流失浓度的影响不显著;不同坡度下径流中总磷(TP)、颗粒态磷(PP)浓度都随着产流时间逐渐变小最后趋于平衡,其中径流中TP主要以PP形式流失,达到80%以上;泥沙中磷素流失主要以无机态磷为主,无机磷分级试验表明被植物高效利用的有效态磷和缓效态磷占无机磷总量的54.1%~57.8%。[结论] 坡度主要通过影响地表径流总量和径流携带的泥沙总量而影响磷素流失总量,石灰土坡耕地磷素流失主要以径流泥沙携带为主。
[Objective] In order to provide basic data for the prevention of agricultural nonpoint source pollution and the protection of water resources in the Three Gorges Reservoir area
the phosphorus loss in regular lime slope farmland under different gradient was researched.[Methods] A sloping farmland in Xiangxi watershed of Three Gorges Reservoir area was selected and an artificial rainfall experiment with rainfall intensity of 1.5 mm/min was conducted. The variations in surface runoff
sediment concentration
total phosphorus(TP) concentration and other forms of inorganic phosphorus were studied.[Results] As the increase of slope
total runoff and sediment increased
whereas
the initial runoff time decreased. However
no significant impact on the sediment concentration was observed. As runoff continued
both TP and particulate phosphorus(PP) decreased and reached a steady concentration under all slope gradients. PP was the primary form of phosphorus loss
accounting for over 80% of that. The inorganic phosphorus suffered the most severe loss for the phosphorus loss of sediment. The inorganic phosphorus grading tests showed that effective phosphorus and slowly available phosphorus accounted for 54.1%~57.8% of the total amount of inorganic phosphorus.[Conclusion] Slope gradient influenced the phosphorus loss through the impacts on surface runoff and sediment loss. The phosphorus of sloping farmland of limestone soil was mainly removed with the sediment.
刘斌涛,陶和平,宋春风,等.1960-2009年中国降雨侵蚀力的时空变化趋势[J].地理研究,2013,32(2):245-255.
赖成光,陈晓宏,王兆礼,等.珠江流域1960-2010年降雨侵蚀力时空变化[J].农业工程学报,2015,31(8):159-167.
胡琳,苏静,桑永枝,等.陕西省降雨侵蚀力时空分布特征[J].干旱区地理,2014,37(6):1101-1107.
Wischmeier W H. A rainfall erosion index for a Universal Soil Loss Equation[J]. Soil Science Society Proceedings, 1959,23(3):246-249.
王万中,焦菊英,郝小品.中国降雨侵蚀力R值的计算与分布Ⅱ[J].水土保持学报,1996,2(1):29-39.
吴德勇,张新.陇东地区降雨侵蚀力时空变化特征分析[J].西北农林科技大学学报:自然科学版,2015,43(6):1-7.
穆兴民,戴海伦,高鹏,等.陕北黄土高原降雨侵蚀力时空变化研究[J],干旱区资源与环境,2010,24(3):37-43.
刘梅,魏加华,王峰.渭河流域降水时空变化与干旱特征分析[J].南水北调与水利科技.2015,13(2):22-27.
马明卫,宋松柏.渭河流域干旱指标空间分布研究[J].干旱区研究,2012,29(4):681-391.
谢元,刘宝元,章文波.侵蚀性降雨标准研究[J].水土保持学报,2000,14(4):6-11.
朱明勇,谭淑端,张全发.近60a汉江流域侵蚀性降雨的时空变化特征[J].生态环境学报,2013,22(9):1544-1549.
章文波,谢元,刘宝元.利用日雨量计算降雨侵蚀力的方法研究[J].地理科学,2002,22(6):705-711.
张家其,龚箭,吴宜进.基于日降雨数据的湖北省降雨侵蚀力初步分析[J].长江流域资源与环境,2014,23(2):274-280.
陈东东,程路,栗晓玮,等.基于地统计学的四川省降雨侵蚀力时空分布特征[J].生态学杂志,2014,33(1):206-213.
刘春利,勤科,谢红霞.延河流域降雨侵蚀力时空分布特征[J].环境科学,2010,31(4):850-857.
汤国安,杨昕.地理信息系统空间分析试验教程[M].北京:科学出版社,2006.
0
浏览量
1097
下载量
1
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621