低温气候下生物刺激烃污染土壤的零度以下土壤CO2呼吸与土壤冻结特性曲线相关。

IF 5.8 3区 环境科学与生态学 0 ENVIRONMENTAL SCIENCES Environmental Science and Pollution Research Pub Date : 2025-01-02 DOI:10.1007/s11356-024-35824-z
Tasnim Nayeema, Aslan Hwanhwi Lee, Amy Richter, Kelvin Tsun Wai Ng, Wonjae Chang
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引用次数: 0

摘要

扩大不冻水的可用性对于寒冷气候下污染土壤的耐应力生物修复至关重要。本研究利用生物刺激、烃类污染的寒冷气候土壤的土壤冻结特性曲线(SFCCs),有效地研究了冻土保水和冻土温度对低温土壤呼吸活性的耦合影响。冻结诱导的土壤呼吸试验是在与现场相关的冻结制度下进行的,程序为4至- 10°C,季节性土壤冻结速率为- 1°C/天。未冻水对土壤呼吸活性延长的影响在土壤冻结开始时就显现出来。未冻水效应在0°C以下变得显著(相关r = 0.83-0.94),与温度效应相当(相关r = 0.82-0.90),成功地证明了对零度以下呼吸活性的耦合效应。仅基于温度依赖性的土壤二氧化碳呼吸模型(Arrhenius和Q10模型)不能准确描述与处理过的污染土壤中未冻水潴留增加相关的零度以下呼吸活性。处理后土壤的sfc位移是土壤温度(T)和未冻水含量(θ)的函数,是有效开发亚零度呼吸模型(sfc - resp)的关键框架。建立的sfc - resp模型非常接近处理后土壤呼吸速率受T和θ影响的变化(R2 = 0.94-0.98),并描述了在深度冻土阶段过渡期间CO2产量的突然减少和随后的稳定。sfc - resp模型与土壤热模型(TEMP/W)相结合,可以得到处理后土壤基质中T、θ和CO2产量的空间分布,为制定耐寒生物修复策略提供了一个近似的工具。
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Sub-zero soil CO2 respiration in biostimulated hydrocarbon-contaminated cold-climate soil can be linked to the soil-freezing characteristic curve

Extending unfrozen water availability is critical for stress-tolerant bioremediation of contaminated soils in cold climates. This study employs the soil-freezing characteristic curves (SFCCs) of biostimulated, hydrocarbon-contaminated cold-climate soils to efficiently address the coupled effects of unfrozen water retention and freezing soil temperature on sub-zero soil respiration activity. Freezing-induced soil respiration experiments were conducted under the site-relevant freezing regime, programmed from 4 to − 10 °C at a seasonal soil-freezing rate of − 1 °C/day. The effects of unfrozen water retention on extending soil respiration activity emerged at the onset of soil-freezing. The unfrozen water effect became significant below 0 °C (correlation r = 0.83–0.94) and comparable to the temperature effect (correlation r = 0.82–0.90), successfully demonstrating the coupled effects on sub-zero respiration activity. Soil CO2 respiration modelling based on the temperature dependency only (Arrhenius and Q10 models) did not accurately describe sub-zero respiration activity associated with increased unfrozen water retention in treated contaminated soils. The shifted SFCCs of the treated soils, expressed as a function of soil temperature (T) and unfrozen water content (θ), served as a key framework for efficiently developing the sub-zero respiration model (SFCC-RESP). The developed SFCC-RESP model closely approximated the changes in soil respiration rates influenced by T and θ in the treated soils (R2 = 0.94–0.98) and described the abrupt decrease and subsequent stabilization in CO2 production during the transition to the deeply frozen soil phase. The SFCC-RESP model integrated with soil thermal models (TEMP/W) can be used to produce spatial distributions of T, θ, and CO2 production in the treated soil matrix, providing a tool to approximate the abundance of unfrozen habitable niches when developing cold-tolerant bioremediation strategies.

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来源期刊
CiteScore
8.70
自引率
17.20%
发文量
6549
审稿时长
3.8 months
期刊介绍: Environmental Science and Pollution Research (ESPR) serves the international community in all areas of Environmental Science and related subjects with emphasis on chemical compounds. This includes: - Terrestrial Biology and Ecology - Aquatic Biology and Ecology - Atmospheric Chemistry - Environmental Microbiology/Biobased Energy Sources - Phytoremediation and Ecosystem Restoration - Environmental Analyses and Monitoring - Assessment of Risks and Interactions of Pollutants in the Environment - Conservation Biology and Sustainable Agriculture - Impact of Chemicals/Pollutants on Human and Animal Health It reports from a broad interdisciplinary outlook.
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