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NET ECOSYSTEM CARBON EXCHANGE AND EVAPOTRANSPIRATION AFTER THE FELLING OF AN EUCALYPTUS FOREST

机译:桉树森林砍伐后净生态系统碳交换和蒸发

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Espirra site (38o38’N,8o36’W) is located in a 300ha Eucalyptus globulus plantation, with a Mediterranean type climate with a mean annual precipitation of 709mm and a mean annual air temperature of 15.9°C. The plantation was established in 1986 with about 1100 trees ha-1. A 33m observation tower was installed in 2002, with an eddy covariance system. A harvesting of trees was made at the end of the 2nd rotation period, from November to December 2006. During the last four years of the second rotation the coppice were 20m height. Harvesting was planned in order to initiate a new 12 year productive cycle. In October 2008 a first thinning was made in three fourths of emerging stems from stumps. At this stage the forest trees had a mean height of 6m. During the period of analyses the total annual precipitation has varied between a minimum of 248mmYr~(-1) (2005) to a maximum of 796mm Yr~(-1) (2007), pattern typical of a Mediterranean climate. The diminution of precipitation (and also how it is distributed along the year) affects the forest uptake of Carbon .The GPP and the TER show lower values in dry years, both in the adult forest as in the young one. The GPP of the growing eucalyptus has been affected by the dry year but also by the thinning that took place in Oct 2008. The Ecosystem total respiration shows high values after the felling ( the same order of magnitude as the forest before the felling) due to the leaves and branches that were left over the soil after the harvesting. Three years after the felling the GPP of the young forest is 61% the value of the adult forest (mean value, excluding the dry year). The seasonal pattern of TER is similar before and after the felling, but in the young forest the GPP is lower and the NEE becomes positive in winter time. In an annual base the growing eucalyptus forest only in the first year after felling was a source of carbon.
机译:Espirta网站(38O38'n,8o36'w)位于300ha桉树球茎种植园,地中海型气候,平均年降水量为709mm,平均年度空气温度为15.9°C。该种植园于1986年建立,约1100年HA-1。 2002年安装了33米观测塔,涡流协方差系统。 11月至2006年11月,在第二次旋转期结束时进行了树木的收获。在过去四年的第二轮旋转期间,COPPICE高度为20米。计划收获以启动新的12年生产周期。 2008年10月,第一次稀释,四分之三的新兴茎从树桩上进行。在这个阶段,森林树的平均高度为6米。在分析期间,年降水量在最小248mmyr〜(-1)(2005)之间变化,最大为796mm Yr〜(-1)(2007),典型的地中海气候。降水量的减少(以及如何沿一年分发)影响碳的森林。GPP和TER在干燥年份显示出较低的数量,既是年轻人的成年林。生长桉树的GPP受到干旱的影响,也受到了2008年10月的稀疏的影响。由于收获后留在土壤上的叶子和树枝。砍伐幼林的GPP后三年是成年森林价值的61%(平均值,不包括干燥年份)。 TER的季节性模式在砍伐之前和之后类似​​,但在年轻的森林中,GPP较低,NEE在冬季变得肯定。在一年一度的基础上,在砍伐之后的第一年生长桉树森林是碳源。

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