Melchior W., Steudle E.
Lehrstuhl fur Pflanzenokologie, Universitat Bayreuth, Postfach 101251, D-8580 Bayreuth, Germany.
Plant Physiol. 1993 Apr;101(4):1305-1315. doi: 10.1104/pp.101.4.1305.
The hydraulic architecture of developing onion (Allium cepa L. cv Calypso) roots grown hydroponically was determined by measuring axial and radial hydraulic conductivities (equal to inverse of specific hydraulic resistances). In the roots, Casparian bands and suberin lamellae develop in the endodermis and exodermis (equal to hypodermis). Using the root pressure probe, changes of hydraulic conductivities along the developing roots were analyzed with high resolution. Axial hydraulic conductivity (Lx) was also calculated from stained cross-sections according to Poiseuille's law. Near the base and the tip of the roots, measured and calculated Lx values were similar. However, at distances between 200 and 300 mm from the apex, measured values of Lx were smaller by more than 1 order of magnitude than those calculated, probably because of remaining cross walls between xylem vessel members. During development of root xylem, Lx increased by 3 orders of magnitude. In the apical 30 mm (tip region), axial resistance limited water transport, whereas in basal parts radial resistances (low radial hydraulic conductivity, Lpr) controlled the uptake. Because of the high axial hydraulic resistance in the tip region, this zone appeared to be "hydraulically isolated" from the rest of the root. Changes of the Lpr of the roots were determined by measuring the hydraulic conductance of roots of different length and referring these data to unit surface area. At distances between 30 and 150 mm from the root tip, Lpr was fairly constant (1.4 x 10-7 m s-1 MPa-1). In more basal root zones, Lpr was considerably smaller and varied between roots. The low contribution of basal zones to the overall water uptake indicated an influence of the exodermal Casparian bands and/or suberin lamellae in the endodermis or exodermis, which develop at distances larger than 50 to 60 mm from the root tip.
通过测量轴向和径向水力传导率(等于比水力阻力的倒数),确定了水培生长的洋葱(Allium cepa L. cv Calypso)发育根系的水力结构。在根系中,凯氏带和栓质化层在内皮层和外皮层(等同于下皮层)中发育。使用根压探针,以高分辨率分析了发育中根系水力传导率的变化。轴向水力传导率(Lx)也根据泊肃叶定律从染色横截面计算得出。在根的基部和尖端附近,测量值和计算值相似。然而,在距根尖200至300毫米的距离处,Lx的测量值比计算值小一个多数量级,这可能是由于木质部导管成员之间残留的横壁所致。在根木质部发育过程中,Lx增加了3个数量级。在根尖30毫米(尖端区域)内,轴向阻力限制了水分运输,而在基部,径向阻力(低径向水力传导率,Lpr)控制了水分吸收。由于尖端区域的轴向水力阻力较高,该区域似乎与根的其余部分“水力隔离”。通过测量不同长度根系的水力导度并将这些数据换算为单位表面积,确定了根系Lpr的变化。在距根尖30至150毫米的距离处,Lpr相当恒定(1.4×10-7米秒-1兆帕-1)。在更靠基部的根区,Lpr要小得多,且不同根系之间存在差异。基部区域对总体水分吸收的贡献较低,这表明内皮层或外皮层中的外皮层凯氏带和/或栓质化层有影响,它们在距根尖大于50至60毫米的距离处发育。