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首页> 外文期刊>Tree Physiology >Fine roots dynamics in a Mediterranean forest: effects of drought and stem density
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Fine roots dynamics in a Mediterranean forest: effects of drought and stem density

机译:地中海森林细根动态:干旱和茎密度的影响

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Summer drought is a characteristic trait of Mediterranean climates and can limit primary production. The holm oak (Quercus ilex L.) forest at the Prades Experimental Complex of Catchments (PECC, NE Spain) was managed by clearcutting until the 1950s. As a result of this practice, the forest has a high density (13000 stems ha~(-1)) that is causing growth stagnation and intense competition for water. A thinning experiment was conducted to release resources, reduce stem competition and improve forest productivity. Minirhizotrons were installed in two plots in each of the thinned and control stands and fine root dynamics quantified to a soil depth of 60 cm over a 2-year period (June 1994-May 1996). Soil water content was higher and soil water penetrated deeper in the soil (30-50 cm) in the thinned plots than in the control plots. In the control plots, soil temperature did not vary substantially with depth (mean = 11.65 deg C), whereas soil temperature was higher in shallow horizons compared with deep horizons in the thinned plots. Mean soil temperature was one degree higher in the thinned plots than in the control plots (12.9 versus 11.9 deg C). There were always more roots in the top 20 cm of soil in thinned plots than in control plots. In the thinned plots, more than 50% of root density (root no. cm~(-2)) was located in the top 20 cm of soil, whereas root density never reached 50% in the 0-20 cm soil layer of the control plots. Roots longevity varied from 35 to 471 days, and there were significant differences between soil depths. Root longevity was greater in the control plots than in the thinned plots.
机译:夏季干旱是地中海气候的特征,可能会限制初级生产。普拉德实验集水区(PECC,西班牙内布拉斯加州)的圣栎林(Quercus ilex L.)森林通过砍伐进行管理,直至1950年代。这种做法的结果是,森林密度高(13000茎ha〜(-1)),导致生长停滞和对水的激烈竞争。进行了间伐试验以释放资源,减少茎秆竞争并提高森林生产力。在2年间(1994年6月至1996年5月),在每个稀疏和对照林分的两个样地中分别安装了小型根际回旋器,并确定了60厘米土壤深度的细根动力学。与对照样地相比,在稀疏地块中,土壤水分含量更高,并且土壤水在土壤中的渗透深度更深(30-50 cm)。在对照样地中,土壤温度并没有随深度变化(平均值= 11.65摄氏度),而在稀疏地带,浅层土壤温度高于深层土壤温度。在稀疏地带,平均土壤温度比对照地带高1度(分别为12.9和11.9摄氏度)。在稀疏地块中,土壤表层20 cm处的根系总是比对照地块中更多。在稀疏的地块中,超过50%的根系密度(根系号cm〜(-2))位于土壤的顶部20 cm,而在0-20 cm的土壤层中,根系密度从未达到50%。控制地块。根的寿命从35天到471天不等,并且土壤深度之间存在显着差异。对照地块的根寿命长于稀疏地块。

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