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Temporal and spatial assessment of evaporation, transpiration, and soil moisture redistribution

机译:蒸发,蒸腾和土壤水分再分布的时空评估

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摘要

At a native stand of creosote bush (Larrea tridentata) in North Las Vegas, a rainfall simulation study was conducted over a 12 month period from October 2005 to October 2006. Simulated rainfall occurred during the winter, spring, summer, and fall periods. Rainfall simulation systems were positioned on each of 12 plots, each containing a single creosote bush. Simulated rainfall events occurred at night with multiple short pulses designed to maximize infiltration while minimizing ponding. Yearly simulated rainfall amounts were set at 0, 15, 30 and 60 cm (replicated three times) and were approximately 0, 1.5, 3.0 and 6.0 times the natural rainfall. The cumulative reference evapotranspiration (ETref) was 156.7 cm and cumulative ambient precipitation was 7.9 cm. Soil and plant canopy surface to air temperature differentials (Ts-Ta and Tc-Ta) were assessed using an infrared thermometer (IRT). Significant differences were based on simulated rainfall treatment (P
机译:在2005年10月至2006年10月的12个月内,对北拉斯维加斯的杂草丛生(Larrea tridentata)进行了降雨模拟研究。模拟的降雨发生在冬季,春季,夏季和秋季。降雨模拟系统位于12个样地中的每个样地上,每个样地都包含一个杂酚丛。模拟的降雨事件在夜间发生,具有多个短脉冲,旨在最大程度地渗透,同时最大程度地减少积水。年度模拟降雨量设定为0、15、30和60 cm(重复三次),约为自然降雨量的0、1.5、3.0和6.0倍。累积参考蒸散量(ETref)为156.7 cm,累积环境降水量为7.9 cm。使用红外测温仪(IRT)评估土壤和植物冠层表面与空气的温差(Ts-Ta和Tc-Ta)。显着差异基于模拟降雨处理(P

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    Bird Brian M.;

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  • 年度 2010
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  • 原文格式 PDF
  • 正文语种 English
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