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红壤区旱地和水田土壤磷素状况及其流失风险
引用本文:肖作义,马飞,柳开楼,赵学强,郑春丽,张昊青,王嘉林,沈仁芳.红壤区旱地和水田土壤磷素状况及其流失风险[J].中国土壤与肥料,2021(1):282-288.
作者姓名:肖作义  马飞  柳开楼  赵学强  郑春丽  张昊青  王嘉林  沈仁芳
作者单位:内蒙古科技大学能源与环境学院;中国科学院南京土壤研究所/土壤与农业可持续发展国家重点实验室;江西省红壤研究所/国家红壤改良工程技术研究中心;中国科学院大学
基金项目:国家自然科学基金项目(31672229);江西省自然科学基金项目(20192BAB203022)。
摘    要:红壤一般偏酸且铁铝富集,磷与铁、铝形成Fe-P、Al-P,降低了红壤磷的有效性.施磷提高红壤供磷能力,但是未被作物利用的磷积累在土壤中,对水体环境构成威胁.研究红壤磷素状况对于提高作物产量和保护环境具有重要意义.已有很多关于红壤磷素状况方面的报道,但是很少将红壤磷素状况与水体磷进行关联分析.在典型红壤区江西省余江县布点...

关 键 词:旱地  水田    流失风险
收稿时间:2019/12/25 0:00:00

Current phosphorus status of red soil in drylands and paddy fields and its loss risks
XIAO Zuo-yi,MA Fei,LIU Kai-lou,ZHAO Xue-qiang,ZHENG Chun-li,ZHANG Hao-qing,WANG Jia-lin,SHEN Ren-fang.Current phosphorus status of red soil in drylands and paddy fields and its loss risks[J].Soil and Fertilizer Sciences in China,2021(1):282-288.
Authors:XIAO Zuo-yi  MA Fei  LIU Kai-lou  ZHAO Xue-qiang  ZHENG Chun-li  ZHANG Hao-qing  WANG Jia-lin  SHEN Ren-fang
Institution:(School of Environment and Energy,Inner Mongolia University of Science and Technology,Baotou Inner Mongolia 014010;State Key Laboratory of Soil and Sustainable Agriculture,Institute of Soil Science,Chinese Academy of Sciences,Nanjing Jiangsu 210008;Jiangxi Institute of Red Soil/National Engineering and Technology Research Center for Red Soil Improvement,Nanchang Jiangxi 330046;University of Chinese Academy of Sciences,Beijing 100049)
Abstract:Red soils are generally acid and contain more Fe and Al that can form Fe-P and Al-P,resulting in low P bioavailability.Applying P fertilizer can improve the capability of red soils to supply P for plants,but the P that is not used by plants accumulates in soils and has potential risks in polluting surface water.Researching soil P status has important implications for increasing crop yield and protecting ecological environment.Much more attention has been paid to the P status of red soils and surface water,but fewer studies pay attention to the direct link between red soil P status and surface water P pollution.We collected 54 soil samples in drylands,54 soil samples in paddy fields and 24 water samples around paddy fields in Yujiang County,Jiangxi Province.We determined the Olsen-P,Bray-P and CaCl2-P concentrations of soil samples,and the total P concentrations of water samples.The results showed that,according to Olsen-P,11%of drylands and 39%of paddy fields were P-deficient,61%of drylands and 39%of paddy fields were P-moderate,and 11%of drylands and 11%of paddy fields were P-excess.According to Bray-P,11%of drylands and 33%of paddy fields were P-deficient,6%of drylands and 33%of paddy fields were P-moderate,and 77%of drylands and 6%of paddy fields were P-excess.A extremely correlation was observed among Olsen-P、Bray-P and CaCl2-P.On the basis of the regressive analyses between Olsen-P and CaCl2-P,and between Bray-P and CaCl2-P,the change points of P loss were 56.31 and 118.4 mg·kg-1 for Olsen-P and Bray-P,respectively.According to the change points,the concentrations of Olsen-P and Bray-P in paddy fields never exceeded the P change point,but 50%and 33%of drylands exceeded the P change points of Olsen-P and Bray-P,respectively.The total P concentrations in the ditches around paddy fields never exceeded the total P standard for surface water in class II of the Environmental Quality Standard for Surface Water.Taken together,dryland soils have high available P concentrations and high P loss risk,whereas paddy soils have low available P concentrations and low P loss risk.
Keywords:dryland  paddy field  phosphorus  loss risks
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