Colombo S J, Asselstine M F
Ontario Tree Improvement and Forest Biomass Institute, Ontario Ministry of Natural Resources, Maple, Ontario, Canada L0J 1E0.
Tree Physiol. 1989 Mar;5(1):73-81. doi: 10.1093/treephys/5.1.73.
The relationship between root elongation and root hydraulic conductivity was investigated in 1-year-old, overwintered black spruce (Picea mariana (Mill.) seedlings. Hydraulic conductivity was estimated by observing water flux through decapitated roots under positive pressure. Five hydraulic conductivity parameters were estimated: (1) water flux under a minimal pressure of 0.2 MPa (J(v, min)); (2) pressure at which a linear relationship between water flux and pressure began (P(min)); (3) slope of the linear water flux-pressure relationship (L(v)); (4) pressure at which the linear relationship between water flux and pressure ended (P(max)); and (5) maximum water flux (J(v, max)). Between day 1 and day 2 after thawing of the growing medium, there were significant increases in L(v) and J(v, max) but there was little, if any, root elongation. Root elongation averaged 5.4 cm seedling(-1) 5 days after thawing and 88.2 cm seedling(-1) 20 days after thawing. Root hydraulic conductivity increased with new root length initially. But between days 20 and 30, when new root length nearly doubled, P(min) was the only measure of hydraulic conductivity that increased significantly. There were significant correlations (P < 0.05) between white root length and both J(v, min) (r(2) = 0.90) and J(v, max) (r(2) = 0.91).
在一年生、经过越冬处理的黑云杉(Picea mariana (Mill.))幼苗中研究了根伸长与根水力传导率之间的关系。通过观察在正压下通过断头根的水流来估计水力传导率。估计了五个水力传导率参数:(1)0.2 MPa最小压力下的水流(J(v, min));(2)水流与压力开始呈线性关系时的压力(P(min));(3)线性水流-压力关系的斜率(L(v));(4)水流与压力线性关系结束时的压力(P(max));以及(5)最大水流(J(v, max))。在生长介质解冻后的第1天到第2天之间,L(v)和J(v, max)显著增加,但根伸长很少(如果有的话)。解冻后5天,根伸长平均为5.4 cm/株,解冻后20天为88.2 cm/株。根水力传导率最初随新根长度增加。但在第20天到第30天之间,当新根长度几乎翻倍时,P(min)是唯一显著增加的水力传导率指标。白根长度与J(v, min)(r(2) = 0.90)和J(v, max)(r(2) = 0.91)之间均存在显著相关性(P < 0.05)。