Development of Acid Sulfate Soil Transformation Models to Manage Disturbed Freshwater Wetlands on Norfolk Island

IF 3.8 2区 农林科学 Q2 SOIL SCIENCE
R. W. Fitzpatrick, B. P. Thomas, S. R. Philip
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引用次数: 0

Abstract

This paper describes models used to explain Acid Sulfate Soil (ASS) transformation processes on Norfolk Island wetlands. Prolonged drying (1970–2020) and a range of human disturbances (from cattle pugging to excavated drains) have led to lower groundwater tables and the formation of Sulfuric organic soils (pH < 4). It builds on a companion paper, which provides the methodological framework by establishing five descriptive soil-landscape models of 14 ASS wetlands affected by anthropogenic disturbances over three drying-wetting cycles (drying until 2020, wetting in 2021, and flooding in 2022). The study aims to enhance land management and improve communication about ASS by applying four simplified soil-landscape models: (1) A descriptive model: Describes processes leading to transformations in the properties of ASS during drying–wetting cycles. It is based on the descriptive models of a range of scenarios presented in the companion paper. (2) An explanatory model: Shows ASS transformation processes, including wetting, drying, and disturbances from excavation and cattle pugging, highlighting reversible and irreversible changes. (3) A predictive (4D) model: Illustrates ASS transformation across diverse environmental conditions, considering three drying–wetting cycles and five disturbance categories. (4) Two predictive evolutionary models: Depicts long-term ASS changes under different conditions, identifying factors that stabilise or accelerate soil changes over recent geological time. These models help non-specialists (such as land holders and community groups) recognise ASS types, monitor changes, and implement either nature-based solutions or remediation management options. They could also be applied to other islands in the south Pacific region.

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诺福克岛受干扰淡水湿地硫酸盐土壤转化模型的建立
本文描述了用于解释诺福克岛湿地酸性硫酸盐土(ASS)转化过程的模型。长期的干旱(1970-2020年)和一系列人为干扰(从放牧到挖掘排水沟)导致地下水位降低和硫有机土壤(pH < 4)的形成。它建立在另一篇论文的基础上,该论文通过建立受三个干湿循环(干燥至2020年,湿润至2021年,洪水至2022年)影响的14个ASS湿地的五个描述性土壤景观模型,提供了方法框架。本文采用四种简化的土壤景观模型:描述模型:描述干湿循环过程中导致土壤性质变化的过程。它是基于配套论文中提出的一系列情景的描述性模型。(2)解释性模型:展示ASS的湿化、干化、开挖干扰和放牧干扰等转化过程,突出可逆和不可逆变化。(3)预测(4D)模型:考虑了3个干湿循环和5种干扰类型,描述了不同环境条件下ASS的变化。(4)两种预测演化模型:描述了不同条件下土壤质量的长期变化,确定了稳定或加速最近地质时期土壤变化的因素。这些模型帮助非专业人员(如土地所有者和社区团体)识别ASS类型,监测变化,并实施基于自然的解决方案或补救管理方案。它们也可适用于南太平洋区域的其他岛屿。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
European Journal of Soil Science
European Journal of Soil Science 农林科学-土壤科学
CiteScore
8.20
自引率
4.80%
发文量
117
审稿时长
5 months
期刊介绍: The EJSS is an international journal that publishes outstanding papers in soil science that advance the theoretical and mechanistic understanding of physical, chemical and biological processes and their interactions in soils acting from molecular to continental scales in natural and managed environments.
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