{"title":"Notice of RetractionPredicting Dissolved Phosphorus Loads from Soil to Runoff in Black Soil, China","authors":"Yang Yuhong, Yan Baixing","doi":"10.1109/ICBBE.2011.5781204","DOIUrl":null,"url":null,"abstract":"Phosphorus is considered to be major limiting factor to freshwater eutrophication. Dissolved phosphorus within soil is the most active component for crop and animal production. Average annual soil loss was 2280 t km-2 by 137Cs technique. A single extraction coefficient was widely used to simulate desorption of phosphorus from soil to runoff. The relation between runoff dissolved phosphorus (y) and soil water-extractable phosphorus (x) is j=0.281x-0.179 (R=0.943). Soil water-extractable phosphorus lost at the rate of 0.371 kg km-2 year-1 during the soil erosion process. Phosphorus loss from soil to runoff was 0.090 kg km-2 year-1. Soil water-extractable phosphorus test is effective for evaluating the potential for soil to release dissolved phosphorus to runoff as the environmentally oriented soil phosphorus test.","PeriodicalId":6438,"journal":{"name":"2011 5th International Conference on Bioinformatics and Biomedical Engineering","volume":"31 1","pages":"1-4"},"PeriodicalIF":0.0000,"publicationDate":"2011-05-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"2011 5th International Conference on Bioinformatics and Biomedical Engineering","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/ICBBE.2011.5781204","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Phosphorus is considered to be major limiting factor to freshwater eutrophication. Dissolved phosphorus within soil is the most active component for crop and animal production. Average annual soil loss was 2280 t km-2 by 137Cs technique. A single extraction coefficient was widely used to simulate desorption of phosphorus from soil to runoff. The relation between runoff dissolved phosphorus (y) and soil water-extractable phosphorus (x) is j=0.281x-0.179 (R=0.943). Soil water-extractable phosphorus lost at the rate of 0.371 kg km-2 year-1 during the soil erosion process. Phosphorus loss from soil to runoff was 0.090 kg km-2 year-1. Soil water-extractable phosphorus test is effective for evaluating the potential for soil to release dissolved phosphorus to runoff as the environmentally oriented soil phosphorus test.
磷被认为是淡水富营养化的主要限制因素。土壤中溶解的磷是作物和动物生产中最活跃的成分。137Cs技术年平均土壤流失量为2280 t km-2。单一提取系数被广泛用于模拟磷从土壤到径流的解吸。径流溶解磷(y)与土壤水可提取磷(x)的关系为j=0.281x-0.179 (R=0.943)。在土壤侵蚀过程中,土壤水可抽取磷的损失速率为0.371 kg km-2 -1。从土壤到径流的磷损失为0.090 kg km-2 -1。土壤水可提取磷试验是评价土壤向径流释放溶解磷潜力的一种环境导向土壤磷试验。