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土壤解冻延迟会影响苏格兰松的根系和地上部分的功能及生长。

Delayed soil thawing affects root and shoot functioning and growth in Scots pine.

作者信息

Repo Tapani, Lehto Tarja, Finér Leena

机构信息

The Finnish Forest Research Institute, Joensuu Research Unit, P.O. Box 68, FI-80101 Joensuu, Finland.

出版信息

Tree Physiol. 2008 Oct;28(10):1583-91. doi: 10.1093/treephys/28.10.1583.

Abstract

In boreal regions, soil can remain frozen after the start of the growing season. We compared relationships between root characteristics and water relations in Scots pine (Pinus sylvestris L.) saplings subjected to soil frost treatments before and during the first week of the growing period in a controlled environment experiment. Delayed soil thawing delayed the onset of sap flow or totally blocked it if soil thawing lagged the start of the growing period by 7 days. This effect was reflected in the electrical impedance of needles and trunks and in the relative electrolyte leakage of needles. Prolonged soil frost reduced or completely inhibited root growth. In unfrozen soil, limited trunk sap flow was observed despite unfavorable aboveground growing conditions (low temperature, low irradiance, short photoperiod). Following the earliest soil thaw, sap flow varied during the growing season, depending on light and temperature conditions, phenological stage of the plant and the amount of live needles in the canopy. The results suggest that delayed soil thawing can reduce tree growth, and if prolonged, it can be lethal.

摘要

在北方地区,生长季节开始后土壤可能仍处于冻结状态。在一项可控环境实验中,我们比较了在生长季第一周之前和期间经历土壤霜冻处理的苏格兰松(Pinus sylvestris L.)幼树根系特征与水分关系之间的联系。土壤解冻延迟会延迟液流开始,或者如果土壤解冻比生长季开始滞后7天,则会完全阻断液流。这种影响体现在针叶和树干的电阻抗以及针叶的相对电解质渗漏上。土壤长时间结霜会减少或完全抑制根系生长。在未冻结的土壤中,尽管地上生长条件不利(低温、低光照、短光周期),仍观察到树干液流有限。最早的土壤解冻之后,液流在生长季会有所变化,这取决于光照和温度条件、植物的物候期以及树冠中活针叶的数量。结果表明,土壤解冻延迟会降低树木生长,如果持续时间延长,可能会导致树木死亡。

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