石灰管理提高美国半干旱地区的土壤 pH 值

Crops & Soils Pub Date : 2024-01-03 DOI:10.1002/crso.20336
Manbir Rakkar, Clain Jones, Perry Miller, Kent McVay, Richard Engel
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引用次数: 0

摘要

土壤酸化是美国和加拿大高降雨量地区的常见问题,在美国西部的半干旱地区,这个问题变得更加普遍。石灰化是缓解土壤酸化的有效方法,因为碳酸盐会与土壤溶液中的氢离子发生反应,从而提高土壤的 pH 值。然而,关于石灰产品的类型、石灰用量、成本效益以及石灰效益的持续时间等问题仍然存在,尤其是在历史上不需要石灰的地区,如大平原的大部分地区。阅读文章并参加 https://web.sciencesocieties.org/Learning-Center/Courses 网站上的测验,可获得 0.5 个水土管理 CEU。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Lime Management to Increase Soil pH in Semi-Arid Regions of the U.S.

Soil acidification, a common issue in high-rainfall areas of the U.S. and Canada, has become a more prevalent problem in the semi-arid areas of the western U.S. Liming is an effective way to mitigate soil acidity as the carbonate reacts with hydrogen ions in the soil solution to increase the soil pH. However, questions exist about the type of liming product, lime rate, cost effectiveness, and how long the lime benefits last, especially in regions that have historically not needed lime, like much of the Great Plains. Earn 0.5 CEUs in Soil & Water Management by reading the article and taking the quiz at https://web.sciencesocieties.org/Learning-Center/Courses.

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