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美国亚利桑那州温带稀树草原树木和草本植物对土壤水分资源的时空分配

Spatial and temporal soil moisture resource partitioning by trees and grasses in a temperate savanna, Arizona, USA.

作者信息

Weltzin Jake F, McPherson Guy R

机构信息

School of Renewable Natural Resources, University of Arizona, 325 Biological Sciences East Building, Tucson, AZ 85721, USA e-mail:

出版信息

Oecologia. 1997 Oct;112(2):156-164. doi: 10.1007/s004420050295.

Abstract

Stable isotope analysis was used to determine sources of water used by coexisting trees and grasses in a temperate savanna dominated by Quercus emoryi Torr. We predicted that (1) tree seedlings and bunchgrasses utilize shallow sources of soil water, (2) mature savanna trees use deeper sources of water, and (3) trees switch from shallow to deep water sources within 1 year of germination. We found that Q. emoryi trees, saplings, and seedlings (about 2 months, 1 year, and 2 years old), and the dominant bunchgrass [Trachypogon montufari (H.B.K.) Nees.] utilized seasonally available moisture from different depths within the soil profile depending on size/age relationships. Sapling and mature Q. emoryi acquired water from >50 cm deep, 2-month-old seedlings utilized water from <15 cm, and 1- and 2-year-old seedlings and grasses used water from between 20 cm and 35 cm. This suggests that very young seedlings are decoupled from grasses in this system, which may facilitate germination and early establishment of Q. emoryi within extant stands of native grasses. The potential for subsequent interaction between Q. emoryi and native grasses was evidenced by similar patterns of soil water use by 1- and 2-year-old seedlings and grasses. Q. emoryi seedlings did not switch from shallow to deep sources of soil water within 2 years of germination: water use by these seedlings apparently becomes independent of water use by grasses after 2 years of age. Finally, older trees (saplings, mature trees) use water from deeper soil layers than grasses, which may facilitate the stable coexistence of mature trees and grasses. Potential shifts in the seasonality of precipitation may alter interactions between woody plants and grasses within temperate savannas characterized by bimodal precipitation regimes: reductions in summer precipitation or soil moisture may be particularly detrimental to warm-season grasses and seedlings of Q. emoryi.

摘要

稳定同位素分析被用于确定在以埃默里栎(Quercus emoryi Torr.)为主的温带稀树草原中共存的树木和草本植物所使用的水源。我们预测:(1)树木幼苗和丛生草本植物利用浅层土壤水源;(2)成熟的稀树草原树木利用深层水源;(3)树木在发芽后1年内从浅层水源切换到深层水源。我们发现,埃默里栎的树木、幼树和幼苗(分别约2个月、1年和2年树龄)以及优势丛生草本植物[蒙图法里草(Trachypogon montufari (H.B.K.) Nees.)]根据大小/年龄关系利用土壤剖面不同深度季节性可得的水分。埃默里栎幼树和成熟树木从深度大于50厘米处获取水分,2个月大的幼苗利用深度小于15厘米处的水分,1年和2年树龄的幼苗以及草本植物利用20厘米至35厘米之间的水分。这表明在该系统中,非常年幼的幼苗与草本植物相互分离,这可能有利于埃默里栎在现存本土草本植物群落中发芽和早期定植。1年和2年树龄的幼苗与草本植物类似的土壤水分利用模式证明了埃默里栎与本土草本植物随后相互作用的可能性。埃默里栎幼苗在发芽后2年内并未从浅层土壤水源切换到深层水源:这些幼苗在2岁之后的水分利用显然变得独立于草本植物的水分利用。最后,较老的树木(幼树、成熟树木)比草本植物利用更深土层的水分,这可能有利于成熟树木和草本植物的稳定共存。降水季节性的潜在变化可能会改变以双峰降水模式为特征的温带稀树草原中木本植物和草本植物之间的相互作用:夏季降水或土壤湿度的减少可能对暖季型草本植物和埃默里栎幼苗特别不利。

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