Boyer J S
College of Marine Studies and College of Agriculture and Natural Resources, University of Delaware, 700 Pilottown Road, Lewes, DE 19958, USA.
J Exp Bot. 2001 Jul;52(360):1483-8. doi: 10.1093/jexbot/52.360.1483.
Multicellular plants display growth-induced water potentials that generate tensions on water in the apoplast and move water into the growing cells. The potentials are sometimes assumed to arise from wall yielding, keeping the turgor pressure below what otherwise would occur. There has been no direct test of this theory, and therefore whole plants or growing regions of stems (hypocotyls) of dark-grown soybean (Glycine max L. Merr.) seedlings were sealed in a pressure chamber, and wall yielding was decreased by applying external pressure. In whole plants, external pressure had little effect because the plants and water supply were uniformly exposed to the pressure. If pressure was applied to the stem while the roots were outside in water, stem elongation was markedly inhibited because the pressure raised the water potential of the growing region and decreased water entry, reducing wall yielding. Further increasing the pressure prevented water entry completely and measured the tensions in the apoplast in the same growing regions. Tensions were about 0.19 MPa at low external pressure, but diminished as wall yielding was inhibited. At external pressures of about 0.63 MPa, wall yielding was abolished and tensions approached zero. There was a linear relation between wall yielding and tension, supporting the theory that wall yielding lowers the turgor thus causing most of the growth-induced water potential.
多细胞植物表现出因生长而产生的水势,这种水势会在质外体中对水产生张力,并使水进入正在生长的细胞。人们有时认为这种水势是由细胞壁屈服产生的,从而使膨压低于原本会出现的水平。尚未对该理论进行直接验证,因此将黑暗中生长的大豆(Glycine max L. Merr.)幼苗的整株植物或茎(下胚轴)的生长区域密封在压力室中,并通过施加外部压力来降低细胞壁屈服。对于整株植物,外部压力影响很小,因为植物和供水都均匀地受到压力作用。如果在根部置于水中时对茎施加压力,茎的伸长会受到明显抑制,因为压力提高了生长区域的水势并减少了水的进入,从而降低了细胞壁屈服。进一步增加压力会完全阻止水的进入,并测量相同生长区域质外体中的张力。在低外部压力下,张力约为0.19兆帕,但随着细胞壁屈服受到抑制而减小。在约0.63兆帕的外部压力下,细胞壁屈服被消除,张力接近零。细胞壁屈服与张力之间存在线性关系,支持了细胞壁屈服会降低膨压从而导致大部分因生长而产生的水势的理论。