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首页> 外文期刊>Hydrological Processes >Using stable isotopes to quantify water sources for trees and shrubs in a riparian cottonwood ecosystem in flood and drought years
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Using stable isotopes to quantify water sources for trees and shrubs in a riparian cottonwood ecosystem in flood and drought years

机译:在干旱和干旱年代,使用稳定同位素量化河岸杨木生态系统中树木和灌木的水源

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摘要

Riparian cottonwood forests in dry regions of western North America do not typically receive sufficient growing season precipitation to completely support their relatively high transpiration requirements. Water used in transpiration by riparian ecosystems must include alluvial groundwater or water stored in the potentially large reservoir of the unsaturated soil zone. We used the stable oxygen and hydrogen isotope composition of stem xylem water to evaluate water sources used by the dominant riparian cottonwood (Populus spp.) trees and shrubs (Shepherdia argentea and Symphoricarpos occidentalis) in Lethbridge, Alberta, during 3 years of contrasting environmental conditions. Cottonwoods did not exclusively take up alluvial groundwater but made extensive use of water sourced from the unsaturated soil zone. The oxygen and hydrogen isotope compositions of cottonwood stem water did not strongly overlap with those of alluvial groundwater, which were closely associated with the local meteoric water line. Instead, cottonwood stem water delta O-18 and delta H-2 values were located below the local meteoric water line, forming a line with a low slope that was indicative of water exposed to evaporative enrichment of heavy isotopes. In addition, cottonwood xylem water isotope compositions had negative values of deuterium excess (d-excess) and line-conditioned (deuterium) excess (lc-excess), both of which provided evidence that water taken up by the cottonwoods had been exposed to fractionation during evaporation. The shrub species had lower values of d-excess and lc-excess than had the cottonwood trees due to shallower rooting depths, and the d-excess values declined during the growing season, as shallow soil water that was taken up by the plants was exposed to increasing, cumulative evaporative enrichment. The apparent differences in functional rooting pattern between cottonwoods and the shrub species, strongly influenced the ratio of net photosynthesis to stomatal conductance (intrinsic water-use efficiency), as shown by variation among species in the delta C-13 values of leaf tissue.
机译:北美西部干旱地区的河岸杨木森林通常不会获得足够的生长季降水来完全满足其相对较高的蒸腾需求。河岸生态系统用于蒸腾的水必须包括冲积地下水或存储在非饱和土壤区潜在的大型水库中的水。我们使用艾伯塔省莱斯布里奇的3年干木质部水的稳定的氧和氢同位素组成来评估主要河岸三叶杨(Populus spp。)乔木和灌木(Shepherdia argentea和Symphoricarpos occidentalis)所使用的水源。三角叶杨不仅仅吸收冲积地下水,而是大量利用了来自非饱和土壤带的水。杨木干水的氧和氢同位素组成与冲积地下水的氧和氢同位素组成没有强烈重叠,而冲积地下水与当地的流水线密切相关。取而代之的是,三角叶杨水的O-18值和H-2值位于局部流水线以下,形成了一个低坡度的线,表明水暴露于重同位素的蒸发富集。此外,杨木木质部水同位素组成的氘过量(d-过量)和线条件(氘)过量(lc-过量)为负值,这两者均提供证据证明三叶杨吸收的水已经暴露于分馏中。在蒸发过程中。由于生根深度较浅,灌木树种的d-过量和lc-过量值均比杨木低,并且由于植物吸收的浅层土壤水暴露,d-过量值在生长季节下降。增加,累积蒸发浓缩。三叶草和灌木物种之间功能性生根模式的明显差异极大地影响了净光合作用与气孔导度的比率(内部水分利用效率),如叶片组织的C-13值之间的差异所表明的。

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