首页> 外文期刊>Revista Brasileira de Ciência do Solo >Establishing environmental soil phosphorus thresholds to decrease the risk of losses to water in soils from Rio Grande do Sul, Brazil
【24h】

Establishing environmental soil phosphorus thresholds to decrease the risk of losses to water in soils from Rio Grande do Sul, Brazil

机译:建立环境土壤磷阈值,降低来自拉西尔苏苏苏廖尔的土壤中损失的风险

获取原文
       

摘要

The overloading of soil with manure or mineral fertilizers enhances phosphorus (P) availability, promoting its loss to water bodies and increasing the risk of eutrophication. In this sense, the establishment of an environmental P threshold is a simple and useful tool to classify soils regards its risk of P losses. Here we propose a P-threshold for soils from the state of Rio Grande do Sul (RS) in Brazil, with the soil clay content as the principal variable of the model. Samples from 20 representative soils of Rio Grande do Sul State were collected in the 0.00-0.10 and 0.10-0.20 m layers. Samples were physically and chemically characterized and incubated with P rates varying from 0 to 100 % of its maximum adsorption capacity. After 20 days of incubation, the P availability was determined in water and Mehlich-1 extractant. We assessed trough segmented linear functions the value of P-Mehlich in which the levels of P water enhance abruptly (i.e., breaking point) to determine the P limit for each soil. Subsequently, the P limit values were linked to the clay content in the sample, adopting the linear equation arising from it as the P-threshold. Adding a safety margin of 20 % to the P-threshold equation, we propose a simplified one “P-threshold = 20 + clay”. Based on the current critical level of P adopted by the regional recommendation in RG, the equation proposed does not limit the production of the most crop species.
机译:用粪肥或矿物肥料的土壤过载增强了磷(P)可用性,促进其对水体的损失并提高富营养化的风险。从这个意义上讲,建立环境P阈值是一种简单而有用的工具,可以对土壤进行分类,以其对P损失的风险。在这里,我们向巴西中Rio Grande Do Sul(Rs)状态的土壤提出了P阈值,土壤粘土含量为模型的主要变量。来自RIO Grande的20个代表性土壤的样品在0.00-0.10和0.10-0.20米的层中收集。物理和化学表征物理和化学表征,并与其最大吸附容量的0%到100%的P速率温育。孵育20天后,在水和Mehlich-1萃取剂中测定P可用性。我们评估了槽分割的线性函数P-Mehlich的值,其中P水的水平突然增强(即,断裂点),以确定每种土壤的P限制。随后,P限制值与样品中的粘土含量连接,采用其作为p阈值引起的线性方程。向P阈值方程添加20%的安全余量,我们提出了一种简化的一个“p阈值= 20 +粘土”。基于RG中区域建议采用的当前临界水平,所提出的等式不限制大多数作物物种的生产。
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号