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模拟大气干旱:硅胶包降低中宇宙微气候的湿度。

Simulating atmospheric drought: Silica gel packets dehumidify mesocosm microclimates.

作者信息

Varghese S, Aguirre B A, Isbell F, Wright A J

机构信息

Department of Biological Sciences California State University Los Angeles Los Angeles California USA.

Department of Ecology, Evolution and Behavior University of Minnesota Minneapolis Minnesota USA.

出版信息

Ecol Evol. 2024 Aug 21;14(8):e70139. doi: 10.1002/ece3.70139. eCollection 2024 Aug.

DOI:10.1002/ece3.70139
PMID:39170050
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11336202/
Abstract

As global temperatures rise, droughts are becoming more frequent and severe. To predict how drought might affect plant communities, ecologists have traditionally designed drought experiments with controlled watering regimes and rainout shelters. Both treatments have proven effective for simulating soil drought. However, neither are designed to directly modify atmospheric drought. Here, we detail the efficacy of a silica gel atmospheric drought treatment in outdoor mesocosms with and without a co-occurring soil drought treatment. At California State University, Los Angeles, we monitored relative humidity, temperature, and vapor pressure deficit every 10 min for 5 months in bare-ground, open-top mesocosms treated with soil drought (reduced watering) and/or atmospheric drought (silica dehumidification packets suspended 12 cm above soil). We found that silica packets dehumidified these mesocosm microclimates most effectively (-5% RH) when combined with reduced soil water, regardless of the ambient humidity levels of the surrounding air. Further, packets increased microclimate vapor pressure deficit most effectively (+0.4 kPa) when combined with reduced soil water and ambient air temperatures above 20°C. Finally, packets simulated atmospheric drought most consistently when replaced within 3 days of deployment. Our results demonstrate the use of silica packets as effective dehumidification agents in outdoor drought experiments. We emphasize that incorporating atmospheric drought in existing soil drought experiments can improve our understandings of the ecological impacts of drought.

摘要

随着全球气温上升,干旱正变得愈发频繁和严重。为了预测干旱可能如何影响植物群落,生态学家传统上通过控制浇水制度和遮雨棚来设计干旱实验。这两种处理方法都已证明对模拟土壤干旱有效。然而,它们都不是为直接改变大气干旱而设计的。在此,我们详细阐述了硅胶大气干旱处理在有或没有同时进行土壤干旱处理的室外中型生态系统中的效果。在加州州立大学洛杉矶分校,我们在经过土壤干旱(减少浇水)和/或大气干旱(在土壤上方12厘米处悬挂硅胶除湿包)处理的裸地、开放式顶部中型生态系统中,每10分钟监测一次相对湿度、温度和水汽压亏缺,持续5个月。我们发现,硅胶包与减少土壤水分相结合时,无论周围空气环境湿度如何,都能最有效地使这些中型生态系统微气候除湿(相对湿度降低5%)。此外,当与减少土壤水分以及高于20°C的环境空气温度相结合时,硅胶包能最有效地增加微气候水汽压亏缺(增加0.4千帕)。最后,硅胶包在部署后3天内更换时能最持续地模拟大气干旱状态。我们的结果证明了硅胶包在室外干旱实验中作为有效除湿剂的用途。我们强调,在现有的土壤干旱实验中纳入大气干旱因素能够增进我们对干旱生态影响的理解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a0b7/11336202/b30fd2af5736/ECE3-14-e70139-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a0b7/11336202/4538639fbec1/ECE3-14-e70139-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a0b7/11336202/d3ef76e023a1/ECE3-14-e70139-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a0b7/11336202/dedd9c44e19f/ECE3-14-e70139-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a0b7/11336202/b30fd2af5736/ECE3-14-e70139-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a0b7/11336202/4538639fbec1/ECE3-14-e70139-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a0b7/11336202/d3ef76e023a1/ECE3-14-e70139-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a0b7/11336202/dedd9c44e19f/ECE3-14-e70139-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a0b7/11336202/b30fd2af5736/ECE3-14-e70139-g001.jpg

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本文引用的文献

1
Atmospheric drying and soil drying: Differential effects on grass community composition.大气干燥和土壤干燥:对草地群落组成的差异影响。
Glob Chang Biol. 2024 Jan;30(1):e17106. doi: 10.1111/gcb.17106.
2
Interactions between beech and oak seedlings can modify the effects of hotter droughts and the onset of hydraulic failure.山毛榉和栎树幼苗之间的相互作用可以改变更热干旱和水力衰竭开始的影响。
New Phytol. 2024 Feb;241(3):1021-1034. doi: 10.1111/nph.19358. Epub 2023 Oct 28.
3
Soil versus atmospheric drought: A test case of plant functional trait responses.
土壤干旱与大气干旱:植物功能性状响应的一个检验案例。
Ecology. 2023 Aug;104(8):e4109. doi: 10.1002/ecy.4109. Epub 2023 Jun 13.
4
Increasing temperature and vapour pressure deficit lead to hydraulic damages in the absence of soil drought.在不存在土壤干旱的情况下,温度和蒸气压亏缺的增加会导致水力损伤。
Plant Cell Environ. 2022 Nov;45(11):3275-3289. doi: 10.1111/pce.14425. Epub 2022 Sep 1.
5
Atmospheric dryness reduces photosynthesis along a large range of soil water deficits.大气干燥会降低在大范围土壤水分亏缺条件下的光合作用。
Nat Commun. 2022 Feb 21;13(1):989. doi: 10.1038/s41467-022-28652-7.
6
Plant responses to rising vapor pressure deficit.植物对不断上升的蒸汽压亏缺的响应。
New Phytol. 2020 Jun;226(6):1550-1566. doi: 10.1111/nph.16485. Epub 2020 Mar 20.
7
Land-atmosphere feedbacks exacerbate concurrent soil drought and atmospheric aridity.陆地-大气反馈加剧了同期土壤干旱和大气干燥。
Proc Natl Acad Sci U S A. 2019 Sep 17;116(38):18848-18853. doi: 10.1073/pnas.1904955116. Epub 2019 Sep 3.
8
Increased atmospheric vapor pressure deficit reduces global vegetation growth.大气水汽压亏缺减少了全球植被生长。
Sci Adv. 2019 Aug 14;5(8):eaax1396. doi: 10.1126/sciadv.aax1396. eCollection 2019 Aug.
9
How ecologists define drought, and why we should do better.生态学家如何定义干旱,以及我们为何应该做得更好。
Glob Chang Biol. 2019 Oct;25(10):3193-3200. doi: 10.1111/gcb.14747. Epub 2019 Jul 19.
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The effect of consumer pressure and abiotic stress on positive plant interactions are mediated by extreme climatic events.消费者压力和非生物胁迫对植物正相互作用的影响是由极端气候事件介导的。
New Phytol. 2018 Jan;217(1):140-150. doi: 10.1111/nph.14778. Epub 2017 Sep 25.