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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Sediment transport due to tree root throw: integrating tree population dynamics, wildfire and geomorphic response
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Sediment transport due to tree root throw: integrating tree population dynamics, wildfire and geomorphic response

机译:树木根系抛弃造成的泥沙迁移:整合树木种群动态,野火和地貌响应

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A field study was conducted to analyze root throw and associated sediment transport in Hawk Creek Watershed, Canadian Rockies. A large crown fire in 2003 allowed the opportunity to study pre-fire and post-fire root throw. Based on field data, a significant relation was found between gradient and root plate volume, as well as individual root plate dimensions. Given that tree diameters increase as trees age and that a relation in the field data was found between tree diameter and root plate volumes, sediment transport clue to root throw is expected to change in response to forest disturbance and stand age. Sediment disturbance, which is the amount of sediment upheaved during tree topple and does not take into account transport distance, shows higher values on steeper gradients. Sediment transport was notable for the steepest plots, with pre-fire values of 0.016 cm(3) cm(-1) a(-1) and post-fire values of 0.18 cm(3) cm(-1) a(-1). A tree population dynamics model is then integrated with a root throw transport model calibrated for the Canadian Rockies to examine the temporal dynamics of sediment transport. Fire is incorporated as a disturbance that initiates development of a new forest, with the model cycling through generations of forest. Trees fall according to an exponential rate that is based on time since death, resulting in a time lag between tree mortality and sediment transport. When values of time-since-previous-fire are short, trees are generally <13 cm, and minimal sediment is upheaved during toppling. If trees reach a critical diameter at breast height (dbh) at time of fire, a pulse of sediment occurs in the immediate post-fire years clue to falling of killed trees, with tree fall rates decreasing exponentially with time-since-fire. A second pulse of root throw begins at about 50 years after the previous fire, once new recruits reach a critical dbh and with initiation of competition-included mortality.
机译:进行了一项野外研究,以分析加拿大洛矶山脉霍克河流域的抛根和相关的泥沙输送。 2003年发生的一次大树冠大火使人们有机会研究大火前和大火后的根部投掷。根据现场数据,发现梯度与根板体积以及各个根板尺寸之间存在显着关系。考虑到树木直径随着树木年龄的增长而增加,并且在野外数据中发现树木直径与根板体积之间存在关系,因此,预计因根源变化而产生的沉积物运输线索会因森林干扰和林分年龄而发生变化。沉积物扰动是树木倒伏过程中沉积物上浮的量,未考虑运输距离,在较陡的坡度上显示出较高的值。沉积物的运输在最陡峭的土地上尤为明显,火灾前的值为0.016 cm(3)cm(-1)a(-1),火灾后的值为0.18 cm(3)cm(-1)a(-1) )。然后将树木种群动态模型与针对加拿大落基山脉进行了校准的根系运输模型相集成,以检查沉积物运输的时间动态。火灾是一种干扰,它引发了新森林的发展,并且模型遍历了几代森林。树木按照自死亡以来的时间的指数速率下降,导致树木死亡与沉积物运输之间存在时间滞后。如果自上一次起火的时间值较短,则树木通常小于13​​厘米,并且在倾倒过程中泥沙流失最少。如果树木在着火时达到胸高(dbh)的临界直径,则在着火后的几年里会出现沉淀物的脉动,这可能是被杀死的树木倒下的原因,树木自倒火以来的掉落率呈指数下降。一旦新兵达到临界dbh并开始包括竞争的死亡率,第二次甩根脉冲就在前一次大火后约50年开始。

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