首页> 外文期刊>The Journal of Applied Ecology >Groundwater salinization intensifies drought impacts in forests and reduces refuge capacity
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Groundwater salinization intensifies drought impacts in forests and reduces refuge capacity

机译:地下水盐碱化加剧干旱在森林和减少影响避难能力

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摘要

Shallow groundwater aquifers regularly support drought refuges for water-dependent ecosystems. However, many aquifers are impacted by over-extraction and pollution, potentially degrading their ability to support groundwater-fed drought refuges. We investigated the response of groundwater-connected riverine forests to a drought considered equivalent in intensity to those predicted under severe climate change for 2030. The drought's impact was investigated in an area where shallow groundwater resources are heavily exploited and polluted by salinization. We used remotely sensed vegetation productivity (enhanced vegetation index) data from a long-term data set (2000-2011) at 475 riverine forest sites in the Campaspe catchment, south-eastern Australia. Generalized additive mixed models and boosted regression trees were used to model the relationship between groundwater and other environmental covariates with forest change during drought. Models explained up to 44% of the variation in forest change during drought. Forests underwent the greatest declines in areas of high salinity (>6000Scm(-1)) associated with shallow groundwater depths (0-5m). Conversely, forests in areas of lowest salinity (<2000Scm(-1)) and groundwater depths of more than 75m showed the least decline during drought. In landscapes where groundwater quality is not compromised, previous studies have shown that shallow groundwater provides important drought refuges and refugia. Here, we show that when groundwater salinization has occurred, forests connected to shallow groundwater are more vulnerable to drought. In effect, salinization reduces the capacity of groundwater-connected habitats to function as drought refuges.Synthesis and applications. Currently, there is an emphasis on managing environmental flows to support freshwater ecosystems and associated forests under water stress. However, delivery of environmental water is restricted to areas within a linear stream network and there is often limited capacity to deliver environmental flows during drought. Alternatively, a focus on drought refuges and refugia and processes important for maintaining groundwater quality (e.g. catchment revegetation to reduce shallow groundwater salinization) may better allow drought effects to be managed across a catchment, without directly focusing on highly contested surface water resources.
机译:浅层地下水含水层定期支持干旱对顾问团在避难所的生态系统。然而,许多地下含水层也受到了影响超采状况和污染,有可能降解能力的支持groundwater-fed干旱避难所。的反应groundwater-connected搁浅森林干旱被认为是等效的恶劣的气候下强度的预测2030年的变化。在一个浅层地下水调查资源利用和污染盐渍化。生产力(增强型植被指数)的数据从一个长期的数据集(2000 - 2011),享年475岁河边的森林站点Campaspe流域,澳大利亚东南部。混合模型和回归树用于模型之间的关系地下水协变量和其他环境与森林变化在干旱。高达44%的森林的变化来解释变化在干旱。领域的高盐度下降幅度最大(> 6000 scm(1))与浅地下水的深度(0-5m)。最低的地区盐度(< 2000 scm(1))和地下水深度超过75了至少在干旱时下降。地下水质量不是妥协,之前研究表明,浅层地下水提供了重要的干旱避难所和聚集地。在这里,我们表明,地下水盐化发生,森林与浅地下水更容易受到干旱。效果,盐渍化降低的能力groundwater-connected栖息地功能干旱避难所。目前,有一种强调管理环境流支持淡水森林生态系统和相关的压力。在一个线性流限制区域网络经常是有限的能力提供在干旱环境流。另外,避难所和关注的干旱对维护生物避难所和过程重要地下水质量(如排水再生长减少浅层地下水盐化)更好的让干旱影响管理一个集水,没有直接专注于高度有争议的地表水资源。

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