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Estimation of water consumption of riparian forest in the lower reaches of Tarim River, northwest China

机译:塔里木河下游沿岸森林耗水量估算

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摘要

The aim of this study is to estimate the water consumption of a Populus euphratica forest. Findings provide a scientific basis for water allocation to the lower reaches of the Tarim River, in Northwest China. In this paper, several different methods were used to gather data. The heat-pulse technique was applied to determine the stem sap flow of P. euphratica sample trees from May to September of 2015. Then, the P. euphratica sapwood area estimation model was established based on the correlation between the sapwood area and the tree biometric parameters. Finally, the water consumption of P. euphratica (n = 3000) trees was calculated. The results showed that the estimated sapwood area of P. euphratica (n = 3000) was 677,000 cm(2), and the total water consumed by these trees during the measurement period was 23,000,000 L. The P. euphratica sap flow varies due to changing environmental factors. The average daily sap flow velocities were 814.3, 1461.75, 1907.27, 1657.51 and 1173.65 mL h(-1) from May to September, respectively. The average daily accumulated sap flow was 22.44, 34.76, 46.98, 40.59 and 32.90 L from May to September, respectively. Pearson correlation analysis showed that variation of sap flow was positively related to solar radiation (R-s) (R-2 = 0.715), air temperature (T-a) (R-2 = 0.744), soil temperature (T-s) (R-2 = 0.806), wind speed (Ws) (R-2 = 0.104). At the same time, sap flow was negatively related to air humidity (H) (R-2 = -0.305). Stepwise regression analysis showed that solar radiation, air temperature, soil temperature and air humidity are the main factors influencing the P. euphratica sap flow variation.
机译:这项研究的目的是估计胡杨林的耗水量。研究结果为中国西北塔里木河下游的配水提供了科学依据。在本文中,使用了几种不同的方法来收集数据。利用热脉冲技术确定了2015年5月至9月的胡杨树干树液流。然后,基于边木面积与树木生物特征之间的相关性,建立了胡杨树液的面积估计模型。参数。最后,计算了胡杨(n = 3000)树木的耗水量。结果表明,估计胡杨的边材面积(n = 3000)为677,000 cm(2),在测量期间这些树木的总耗水量为23,000,000L。胡杨的树液流量因变化而变化环境因素。从5月到9月,平均日树液流速分别为814.3、1461.75、1907.27、1657.51和1173.65 mL h(-1)。 5月至9月,平均日累积树液流量分别为22.44、34.76、46.98、40.59和32.90L。皮尔逊相关分析表明,汁液流量的变化与太阳辐射(Rs)(R-2 = 0.715),气温(Ta)(R-2 = 0.744),土壤温度(Ts)(R-2 = 0.806)呈正相关。 ),风速(Ws)(R-2 = 0.104)。同时,树液流量与空气湿度(H)呈负相关(R-2 = -0.305)。逐步回归分析表明,太阳辐射,气温,土壤温度和空气湿度是影响胡杨液流变化的主要因素。

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  • 来源
    《Environmental earth sciences》 |2017年第16期|547.1-547.11|共11页
  • 作者单位

    Xinjiang Univ, Coll Resources & Environm Sci, Key Lab Oasis Ecol, Urumqi 830046, Peoples R China;

    Xinjiang Univ, Coll Resources & Environm Sci, Key Lab Oasis Ecol, Urumqi 830046, Peoples R China|Catholic Univ Eichstaett Ingolstadt, Fac Math & Geog, D-85072 Eichstatt, Germany;

    Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Urumqi 830046, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Tarim River; Populus euphratica; Sap flow; Sapwood area; Upscaling;

    机译:塔里木河;胡杨;树干液流;边材面积;放大;

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