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1
Postfire soil water repellency in piñon-juniper woodlands: Extent, severity, and thickness relative to ecological site characteristics and climate.矮松-杜松林地火灾后土壤斥水性:与生态立地特征和气候相关的范围、严重程度及厚度
Ecol Evol. 2017 May 22;7(13):4630-4639. doi: 10.1002/ece3.3039. eCollection 2017 Jul.
2
Mapping "old" vs. "young" piñon-juniper stands with a predictive topo-climatic model.使用预测性地形气候模型绘制“老龄”与“年轻”矮松-杜松群落分布图。
Ecol Appl. 2008 Oct;18(7):1627-41. doi: 10.1890/07-0847.1.
3
Woodland recovery following drought-induced tree mortality across an environmental stress gradient.干旱诱发树木死亡后,林地在环境胁迫梯度上的恢复。
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4
Tree regeneration following drought- and insect-induced mortality in piñon-juniper woodlands.干旱和虫害导致的雌雄松林死亡后的树木再生。
New Phytol. 2013 Oct;200(2):402-412. doi: 10.1111/nph.12366. Epub 2013 Jun 17.
5
Prolonged experimental drought reduces plant hydraulic conductance and transpiration and increases mortality in a piñon-juniper woodland.长期的实验干旱降低了植物的水力传导率和蒸腾作用,并增加了刺柏林地的死亡率。
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J Environ Qual. 2003 Jul-Aug;32(4):1290-8.
8
Historical fire and multidecadal drought as context for piñon-juniper woodland restoration in western Colorado.以历史火灾和数十年干旱为背景探讨科罗拉多州西部矮松-杜松林地的恢复
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Fine-scale stand structure mediates drought-induced tree mortality in pinyon-juniper woodlands.细尺度林分结构调节了刺柏林地中干旱引起的树木死亡。
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本文引用的文献

1
Temporal changes in soil water repellency after a forest fire in a Mediterranean calcareous soil: Influence of ash and different vegetation type.林火后石灰性土壤持水能力的时间变化:灰分和不同植被类型的影响。
Sci Total Environ. 2016 Dec 1;572:1252-1260. doi: 10.1016/j.scitotenv.2015.09.121. Epub 2015 Oct 1.
2
Effects of climate change on the delivery of soil-mediated ecosystem services within the primary sector in temperate ecosystems: a review and New Zealand case study.气候变化对温带生态系统初级部门土壤介导生态系统服务提供的影响:综述与新西兰案例研究。
Glob Chang Biol. 2015 Aug;21(8):2844-60. doi: 10.1111/gcb.12949. Epub 2015 Jun 8.
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Feature extraction techniques for measuring piñon and juniper tree cover and density, and comparison with field-based management surveys.用于测量刺柏和杜松树冠和密度的特征提取技术,以及与基于实地的管理调查的比较。
Environ Manage. 2011 May;47(5):766-76. doi: 10.1007/s00267-011-9634-3. Epub 2011 Mar 1.
4
Higher trends but larger uncertainty and geographic variability in 21st century temperature and heat waves.21世纪气温和热浪呈上升趋势,但不确定性更大且存在地理差异。
Proc Natl Acad Sci U S A. 2009 Sep 15;106(37):15555-9. doi: 10.1073/pnas.0904495106. Epub 2009 Sep 8.
5
Should we always choose a nonparametric test when comparing two apparently nonnormal distributions?当比较两个明显非正态分布时,我们是否应该总是选择非参数检验?
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矮松-杜松林地火灾后土壤斥水性:与生态立地特征和气候相关的范围、严重程度及厚度

Postfire soil water repellency in piñon-juniper woodlands: Extent, severity, and thickness relative to ecological site characteristics and climate.

作者信息

Zvirzdin Daniel L, Roundy Bruce A, Barney Nicholas S, Petersen Steven L, Anderson Val J, Madsen Matthew D

机构信息

Bureau of Land Management Elko NV USA.

Department of Plant and Wildlife Sciences Brigham Young University Provo UT USA.

出版信息

Ecol Evol. 2017 May 22;7(13):4630-4639. doi: 10.1002/ece3.3039. eCollection 2017 Jul.

DOI:10.1002/ece3.3039
PMID:28690793
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5496519/
Abstract

Wildfires can create or intensify water repellency in soil, limiting the soil's capacity to wet and retain water. The objective of this research was to quantify soil water repellency characteristics within burned piñon-juniper woodlands and relate this information to ecological site characteristics. We sampled soil water repellency across forty-one 1,000 m study plots within three major wildfires that burned in piñon-juniper woodlands. Water repellency was found to be extensive-present at 37% of the total points sampled-and strongly related to piñon-juniper canopy cover. Models developed for predicting SWR extent and severity had values of 0.67 and 0.61, respectively; both models included piñon-juniper canopy cover and relative humidity the month before the fire as coefficient terms. These results are important as they suggest that postfire water repellency will increase in the coming years as infilling processes enhance piñon-juniper canopy cover. Furthermore, reductions in relative humidity brought about by a changing climate have the potential to link additively with infilling processes to increase the frequency and intensity of wildfires and produce stronger water repellency over a greater spatial extent. In working through these challenges, land managers can apply the predictive models developed in this study to prioritize fuel control and postfire restoration treatments.

摘要

野火会导致土壤产生或增强斥水性,限制土壤的湿润和保水能力。本研究的目的是量化火烧矮松-杜松林土壤的斥水特性,并将这些信息与生态立地特征联系起来。我们在矮松-杜松林发生的三场主要野火中,对41个1000平方米的研究地块的土壤斥水性进行了采样。发现斥水性广泛存在,在采样点总数的37%处存在,且与矮松-杜松林冠层覆盖密切相关。用于预测土壤斥水范围和严重程度的模型的 值分别为0.67和0.61;两个模型均将矮松-杜松林冠层覆盖和火灾前一个月的相对湿度作为系数项。这些结果很重要,因为它们表明,随着林分郁闭过程增强矮松-杜松林冠层覆盖,未来几年火灾后的斥水性将会增加。此外,气候变化导致的相对湿度降低有可能与林分郁闭过程相加作用,增加野火的频率和强度,并在更大空间范围内产生更强的斥水性。在应对这些挑战时,土地管理者可以应用本研究中开发的预测模型,对燃料控制和火灾后恢复处理进行优先排序。