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Prospects for smart soil management techniques in grazing systems - techniques and implications of spatial management of grassland soils

机译:放牧系统中智能土壤管理技术的前景 - 草地土壤空间管理的技术与含义

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摘要

Precision management of nutrient input to grazing systems offers the opportunity to optimise pasture production whilst minimising environmental impacts.Grazed grasslands are associated with highly heterogeneous soil properties that develop as a consequence of uneven distribution of dung and urine deposition, differences in underlying topography, and variations in soils and microclimates. This heterogeneity leads to variability in plant growth, nutrient usage efficiency, and nutrient (particularly nitrogen) losses. Despite this, it is conventional to manage fields uniformly when adding nutrients or lime leading to inefficient nutrient use. Development of spatially variable inputs to grasslands requires an understanding of the spatial distribution of underlying soil properties, and the way in which they influence soil and plant nutrient cycling. This paper provides an overview of the variations in soilfertility that contributes to uneven nutrient use efficiency, and using the example of variations in soil pH, assesses the extent to which spatially variable applications of ' lime could be predicted to influence pasture production, and greenhouse gas emissions.
机译:放牧系统的营养输入的精确管理提供了优化牧场生产的机会,同时最大限度地减少环境影响。Gradled草原与高度异质的土壤性质相关,这些土壤性质与粪便分布的不均匀分布,潜在地形的差异和变化的结果有关。在土壤和微亚亚麻层中。这种异质性导致植物生长,营养使用效率和营养素(特别是氮气)损失的可变性。尽管如此,当添加营养或石灰时,它是统一的统一管理领域,导致营养素低效。对草原的空间可变输入的发展需要了解潜在土壤性质的空间分布,以及它们影响土壤和植物营养循环的方式。本文概述了散发性的变化,有助于不均匀的营养利用效率,并使用土壤pH的变化的例子,评估'石灰可以预测影响牧场生产的空间可变应用的程度,以及温室气体排放。

著录项

  • 来源
    《Advances in Animal Biosciences》 |2017年第3期|共1页
  • 作者单位

    Scotland's Rural College Edinburgh UK;

    Scotland's Rural College Edinburgh UK;

    Centre for Ecology and Hydrology Edinburgh UK;

    Scotland's Rural College Edinburgh UK;

    Centre for Ecology and Hydrology Edinburgh UK;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 动物学;
  • 关键词

  • 入库时间 2022-08-20 00:34:30

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