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Ozone concentrations, flux and potential effect on yield during wheat growth in the Northwest-Shandong Plain of China

机译:鲁西北平原小麦生长过程中臭氧浓度,通量及对产量的潜在影响

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摘要

Ozone (O-3) concentration and flux (F-o) were measured using the eddy covariance technique over a wheat field in the Northwest-Shandong Plain of China. The O-3-induced wheat yield loss was estimated by utilizing O-3 exposure-response models. The results showed that: (1) During the growing season (7 March to 7 June, 2012), the minimum (16.1 ppbV) and maximum (53.3 ppbV) mean O-3 concentrations occurred at approximately 6:30 and 16:00, respectively. The mean and maximum of all measured O-3 concentrations were 31.3 and 128.4 ppbV, respectively. The variation of O-3 concentration was mainly affected by solar radiation and temperature. (2) The mean diurnal variation of deposition velocity (V-d) can be divided into four phases, and the maximum occurred at noon (12: 00). Averaged V-d during daytime (6:00-18:00) and nighttime (18:00-6:00) were 0.42 and 0.14 cm/sec, respectively. The maximum of measured V-d was about 1.5 cm/sec. The magnitude of V-d was influenced by the wheat growing stage, and its variation was significantly correlated with both global radiation and friction velocity. (3) The maximum mean Fo appeared at 14:00, and the maximum measured F-o was -33.5 nmol/(m(2).sec). Averaged Fo during daytime and nighttime were -6.9 and -1.5 nmol/(m(2).sec), respectively. (4) Using O-3 exposure-response functions obtained from the USA, Europe, and China, the O-3-induced wheat yield reduction in the district was estimated as 12.9% on average (5.5%-23.3%). Large uncertainties were related to the statistical methods and environmental conditions involved in deriving the exposure-response functions. (C) 2015 The Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences. Published by Elsevier B.V.
机译:使用涡度协方差技术测量了中国西北-山东平原麦田中的臭氧(O-3)浓度和通量(F-o)。利用O-3暴露-响应模型估算了O-3诱导的小麦单产损失。结果表明:(1)在生长季节(2012年3月7日至6月7日),O-3的最低(16.1 ppbV)和最高(53.3 ppbV)平均浓度分别出现在大约6:30和16:00,分别。所有测得的O-3浓度的平均值和最大值分别为31.3和128.4 ppbV。 O-3浓度的变化主要受太阳辐射和温度的影响。 (2)沉积速度的平均日变化(V-d)可以分为四个阶段,最大值出现在中午(12:00)。白天(6:00-18:00)和夜间(18:00-6:00)的平均V-d分别为0.42和0.14 cm / sec。测量的V-d的最大值约为1.5cm / sec。 V-d的大小受小麦生育期的影响,其变化与总体辐射和摩擦速度均显着相关。 (3)最大平均Fo出现在14:00,并且最大测量的F-o为-33.5nmol /(m(2).sec)。白天和晚上的平均Fo分别为-6.9和-1.5 nmol /(m(2).sec)。 (4)使用从美国,欧洲和中国获得的O-3暴露-响应函数,估计该地区O-3诱导的小麦减产平均为12.9%(5.5%-23.3%)。很大的不确定性与推导暴露响应函数所涉及的统计方法和环境条件有关。 (C)2015中国科学院生态环境研究中心。由Elsevier B.V.发布

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