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首页> 外文期刊>Agricultural and Forest Meteorology >Above- and belowground ecosystem biomass and carbon pools in an age-sequence of temperate pine plantation forests.
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Above- and belowground ecosystem biomass and carbon pools in an age-sequence of temperate pine plantation forests.

机译:温带松树人工林年龄序列中地上和地下生态系统的生物量和碳库。

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摘要

We assessed the successional development of above- and belowground ecosystem biomass and carbon (C) pools in an age-sequence of four White pine (Pinus strobus L.) plantation stands (2-, 15-, 30-, and 65-years-old) in Southern Ontario, Canada. Biomass and C stocks of above- and belowground live and dead tree biomass, understorey and forest ground vegetation, forest floor C (LFH-layer), and woody debris were determined from plot-level inventories and destructive tree sampling. Small root biomass (5 mm) and mineral soil C stocks were estimated from soil cores. Aboveground tree biomass became the major ecosystem C pool with increasing age, reaching 0.5, 66, 92, and 176 t ha-1 in the 2-, 15-, 30-, and 65-year-old stands, respectively. Tree root biomass increased from 0.1 to 10, 18, 38 t ha-1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, contributing considerably to the total ecosystem C in the three older stands. Forest floor C was 0.8, 7.5, 5.4, and 12.1 t C ha-1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, indicating an increase during the first two decades, but no further age-effect during the later growth phase. Mineral soil C was age-independent with 37.2, 33.9, 39.1, and 36.7 t C ha-1 in the 2-, 15-, 30-, and 65-year-old stands, respectively. Aboveground ecosystem C increased with age from 3 to 40, 52, and 100 t C ha-1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, due to an increase in aboveground tree biomass. Belowground ecosystem C remained similar in the early decades after establishment with 37, 39, and 39 t C ha-1 in the 2-, 15-, and 30-year-old stands, but increased to 56 t C ha-1 in the 65-year-old stand due to an increase in root biomass. The difference in total ecosystem C between the 2- and 65-year-old stand was 116 t C ha-1. Our results highlight the importance of considering the successional development of forest ecosystem C pools, when estimating C sink potentials over their complete life cycle..
机译:我们评估了四个白松(Pinus strobus L.)人工林(2年,15年,30年和65年)的年龄序列中地上和地下生态系统生物量和碳(C)库的连续发展。老)在加拿大安大略省南部。从地块级清单和破坏性树木抽样中确定了地上和地下活树和枯树生物量,地下和森林地面植被,林地C(LFH层)和木屑的生物量和碳储量。从土壤核心估算出小的根系生物量(<5毫米)和矿质土壤碳储量。地上树木生物量随着年龄的增长成为主要的生态系统碳库,在2、15、30和65岁的林分中分别达到0.5、66、92和176 t ha-1。在2、15、30和65岁的林分中,树根的生物量分别从0.1增加到10、18、38 t ha-1,这在三个较早的林分中对整个生态系统C的贡献很大。在2、15、30和65岁的林分中,林地C分别为0.8、7.5、5.4和12.1 t C ha-1,表明在最初的20年中有所增加,但是没有进一步的增加。后期生长阶段的年龄效应。矿物土壤C与年龄无关,分别在2、15、30和65岁的林分中分别具有37.2、33.9、39.1和36.7 t C ha-1。在2、15、30和65岁的林分中,地上生态系统C随着年龄的增长从3 t分别增加到40、52和100 t C ha-1,这是由于地上树木生物量的增加所致。地下生态系统C在建立后的最初几十年中仍然相似,分别在2、15和30年的林分中分别具有37、39和39 t C ha-1,但在第二年,15和30年的林分中增加到56 t C ha-1。根部生物量增加,使树龄达到65岁。 2岁和65岁林分之间的总生态系统碳差异为116 t C ha-1。我们的结果凸显了在估算整个生命周期中的碳汇潜力时,考虑森林生态系统碳库的连续发展的重要性。

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