Redmann R E
Plant Ecology Department, University of Saskatchewan, S7N OWO, Saskatoon, Sask., Canada.
Oecologia. 1976 Dec;23(4):283-295. doi: 10.1007/BF00345958.
Seasonal and diurnal patterns of osmotic and leaf water potential of several mixed grassland species were studied. The osmotic potential (OP) of Agropyron dasystachyum ranged from about-15 bars early in the growing season to about-30 bars during late summer droughts. Seasonal trends in A. smithii and Koeleria cristata were similar. Minimum osmotic potentials of Eurotia lanata and Artemisia frigida were-42 and-35 bars, respectively. The mesophytes Geum triflorum and Lomatium foeniculaceum did not exhibit OP below-20 bars. Soil water, particularly in the 0-15 cm layer, strongly influenced OP and leaf water potential (WP). Seasonal trends in WP were similar to OP. Under low stress, WP was about 10 bars greater than OP; under high stress WP was equal or even lower then OP (negative turgor). Diurnal fluctuations in WP were greater than those of OP when low stress conditions existed. Diurnal changes in potential were related to global radiation which was an index of atmospheric evaporative demand. Ecological implications of water status are discussed.
研究了几种混合草地物种渗透势和叶片水势的季节和昼夜模式。糙野麦的渗透势(OP)在生长季节早期约为-15巴,在夏末干旱期间约为-30巴。史密斯冰草和猬草的季节趋势相似。绵毛优若藜和冷蒿的最低渗透势分别为-42巴和-35巴。中生植物三花水杨梅和丝叶裂叶芹的渗透势未低于-20巴。土壤水分,特别是0-15厘米土层的土壤水分,对渗透势和叶片水势(WP)有强烈影响。叶片水势的季节趋势与渗透势相似。在低胁迫下,叶片水势比渗透势高约10巴;在高胁迫下,叶片水势等于或甚至低于渗透势(负膨压)。在低胁迫条件下,叶片水势的昼夜波动大于渗透势。势的昼夜变化与全球辐射有关,全球辐射是大气蒸发需求的一个指标。讨论了水分状况的生态意义。