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中欧地区云杉树冠(欧洲云杉)对二氧化硫、一氧化氮和臭氧的气孔吸收及冠层损害

Stomatal uptake of SO , NO and O by spruce crowns (Picea abies) and canopy damage in Central Europe.

作者信息

Slovik Stefan, Siegmund Alfred, Führer Hans-Werner, Heber Ulrich

机构信息

Julius-von-Sachs-Institut für Biowissenschaften mit Botanischem Garten der Unversität Würzburg, Lehrstuhf für Botanik I, Mittlerer Dallenbergweg 64, 97082 Würzburg, Germany.

Hessische Landensanstalt für Umwelt, P.O. Box 3209, 65022 Wiesbaden, Rheingaustraβe 186, 65203 Wiesbaden, Germany.

出版信息

New Phytol. 1996 Apr;132(4):661-676. doi: 10.1111/j.1469-8137.1996.tb01884.x.

Abstract

The stomatal uptake of SO , NO and O by Norway spruce canopies (Picea abies (L.) Karst.) has been integrated at six sites in central Germany (Königstein in the Taunus mountains. Witzenhausen, Grebenau, Frankenberg, Fürth in the Odenwald mountains and Biebergemünd in the Spessart mountains), Results are based on 788000 half-hourly available sets of field data on air pollution and site meteorology measured since 1984 (45 site years). Data on stomatal water conductance are available from statistical response functions obtained in the field at all times of day and seasons of the year. From this, stomatal conductance was calculated fur different atmospheric tract gases. Statistical response functions are presented which allow the separate estimation of annual stomatal net uptake of trace gases in the field if only (i) measured annual means of SO , NO , and O , pollution and (ii) the length of the trunk growth period (defined by temperature) are known. The following specific annual doses of stomatal trace-gas net uptake in the field (μmol m total needle surface d annual trunk growth period/(nPa Pa ) annual mean of trace gas concentration) are obtained; SO : (0.157 ± 0.011) μmol m d /(nPa SO , Pa ), NO : (0.4774 ± 0.034) μmol m d /(nPa NO Pa ), O : (0.474 ± 0.034) μmol m d /(nPa O Pa ). There is an apparent NO , compensation point at 7 nPa Pa in the field if NO (=NO , + NO) fluxes are integrated; the individual NO , compensation point equals c 3.2 nPa Pa . Additionally, a statistical response function is presented, which estimates actual stomatal water transpiration rates in the field on the basis of measured water vapour pressure differences. VPD (mPa Pa ). Complex canopy effects were calculated on the basis of available data using an effective leaf area which is 0×32 times the morphological leaf area index. Results are consistent (i) with available water balance data, (ii) with observed SO -dependent sulphate accumulation rates in spruce needles and (iii) with observed epicuticular SO , deposition rates. Pollution data are compared with observed damage of spruce canopies in the field. There was a statistically significant correlation between observed damage to spruce canopies.

摘要

对德国中部六个地点(陶努斯山脉的柯尼希施泰因、维岑豪森、格雷贝瑙、弗兰肯贝格、奥登瓦尔德山脉的菲尔特以及施佩萨特山脉的比贝格明德)的挪威云杉林冠层(欧洲云杉(Picea abies (L.) Karst.))对二氧化硫、一氧化氮和臭氧的气孔吸收进行了综合研究。结果基于自1984年以来测量的788000组每半小时一次的空气污染和场地气象的现场数据(45个场地年)。气孔导水率数据可从一年中所有时间和季节在现场获得的统计响应函数中获取。据此,计算了不同大气痕量气体的气孔导度。给出了统计响应函数,仅在已知(i)二氧化硫、一氧化氮和臭氧污染的年测量平均值以及(ii)树干生长周期长度(由温度定义)的情况下,可单独估算现场痕量气体的年气孔净吸收量。得到了以下现场痕量气体气孔净吸收的特定年剂量(微摩尔每平方米针叶总面积每天树干生长周期/(纳帕斯卡帕)痕量气体浓度年平均值):二氧化硫:(0.157±0.011)微摩尔每平方米每天/(纳帕二氧化硫帕斯卡),一氧化氮:(0.4774±0.034)微摩尔每平方米每天/(纳帕一氧化氮帕斯卡),臭氧:(0.474±0.034)微摩尔每平方米每天/(纳帕臭氧帕斯卡)。如果对一氧化氮(=一氧化氮+二氧化氮)通量进行积分,现场存在一个明显的二氧化氮补偿点,为7纳帕斯卡帕;单个二氧化氮补偿点约为3.2纳帕斯卡帕。此外,还给出了一个统计响应函数,该函数根据测量的水汽压差(VPD,毫帕斯卡帕)估算现场实际的气孔水分蒸腾速率。基于现有数据,使用有效叶面积(为形态叶面积指数的0.32倍)计算了复杂的林冠层效应。结果(i)与现有水平衡数据一致,(ii)与云杉针叶中观察到的依赖二氧化硫的硫酸盐积累速率一致,(iii)与观察到的表皮二氧化硫沉积速率一致。将污染数据与现场观察到的云杉林冠层损伤进行了比较。观察到的云杉林冠层损伤之间存在统计学上的显著相关性。

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