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首页> 外文期刊>Canadian Journal of Forest Research >Effects of harvesting and drought on CO2 and H2O fluxes in an aspen-dominated western boreal plain forest: early chronosequence recovery
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Effects of harvesting and drought on CO2 and H2O fluxes in an aspen-dominated western boreal plain forest: early chronosequence recovery

机译:采伐和干旱对以杨木为主的西部北方平原森林CO2和H2O通量的影响:早期时序恢复

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This study examines the hydrological recovery of two regenerating boreal trembling aspen (Populus tremuloides Michx.) dominated stands and the sensitivity of that regeneration to drought within the first 5 years of establishment. The results indicate that evapotranspiration fluxes and water-use efficiency rebounded quickly as a result of new vegetation foliage growth and wet conditions found within the first 2 years following the harvest. However, a period of dry years had a significant influence on rates of postharvest growth, carbon dioxide (CO2), and water fluxes at these sites. The northern study area (NSA) and southern study area (SSA) were harvested in the winters of 2007 and 2008, respectively. The first and second years of regeneration at the SSA and NSA, respectively, were marked by an early spring thaw and higher-than-normal precipitation, while air temperatures remained slightly above the 30-year normal. During this period, mean measured height of vegetation tripled at both sites, and cumulative evapotranspiration was approximately 60% of that prior to harvest by the end of the second year of growth. By the third year (2009), the NSA became a sink for atmospheric CO2 during the snow free season (days of the year 128-238) despite low precipitation during the latter half of the summer. Volumetric soil moisture content in 2009 was the highest (on average) of the 5 years examined due to heavy snowfall and a late start to the growing season (where air temperatures consistently exceeded 0 degrees C), resulting in sustained productivity. However, cumulative annual precipitation also declined to 79% and 57% in 2009 and 2010, respectively, of the 30-year normal for that region, leading to significant (lagged) declines in forest productivity at the NSA in 2010 and 2011. This resulted in the site becoming a source of CO2 to the atmosphere during the 2010 and 2011 growing seasons (annual balance was not measured). Throughout the drought period (2009, 2010, and 2011), mean stand height increased by only 15%, 11%, and 14%, respectively, compared with the mean stand height in 2008. Water-use efficiency also declined in 2010 and 2011, whereas differences in light-use efficiency did not vary significantly because foliage was maintained (i.e., leaves did not abscise as a result of drought). The results of this study indicate that regenerating aspen stands are sensitive to drought and respond relatively quickly to changes in the soil moisture regime. This is important because regional drying as a result of predicted climatic changes combined with increased industrial activity may result in significant decline in productivity within these stands over broad regions.
机译:这项研究研究了在建立的头5年内,两个再生的北方颤抖白杨(Populus tremuloides Michx。)为主的林分的水文恢复以及该再生对干旱的敏感性。结果表明,由于收获后头两年内出现了新的植被叶子生长和潮湿条件,蒸散发通量和水分利用效率迅速回升。然而,干旱的时期对这些地点的采后生长速率,二氧化碳(CO2)和水通量有重大影响。北部研究区(NSA)和南部研究区(SSA)分别于2007年和2008年冬季收获。 SSA和NSA再生的第一年和第二年分别以春季早融化和高于正常水平的降水为标志,而空气温度仍略高于30年正常值。在此期间,两个地点的植被平均测量高度增加了两倍,到生长的第二年年底,累计蒸散量约为收获前的蒸散量的60%。到第三年(2009年),尽管夏季后半段降雨少,但NSA在无雪季节(128-238年的日子)期间已成为大气CO2的汇入点。由于下大雪和生长季节的开始较晚(气温持续超过0摄氏度),2009年的土壤含水量最高(平均)为5年中最高(平均),从而实现了持续的生产力。但是,该地区30年正常值的累计年度降水量在2009年和2010年也分别降至79%和57%,导致2010年和2011年NSA的森林生产力显着(滞后)下降。在2010年和2011年生长季节期间,该站点成为大气中的CO2来源(未测量年平衡)。在整个干旱时期(2009年,2010年和2011年),平均林分高度与2008年的平均林分高度相比仅分别增加了15%,11%和14%。2010年和2011年的用水效率也有所下降,而光利用效率的差异并没有显着变化,这是因为维持了枝叶(即,叶片没有因干旱而缺席)。这项研究的结果表明,再生的白杨林对干旱敏感,对土壤水分状况的变化反应相对较快。这很重要,因为由于预期的气候变化以及工业活动的增加而导致的区域干燥可能会导致这些大面积林分的生产力显着下降。

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