Lavigne M B, Foster R J, Goodine G
Natural Resources Canada, Canadian Forest Service--Atlantic Forestry Centre, Fredericton, NB E3B 5P7, Canada.
Tree Physiol. 2004 Apr;24(4):415-24. doi: 10.1093/treephys/24.4.415.
Soil respiration (rs), soil temperature (Ts) and volumetric soil water content were measured in a balsam fir (Abies balsamea (L.) Mill.) ecosystem from 1998 to 2001. Seasonal variation in root and microbial respiration, and covariation in abiotic factors confounded interpretation of the effects of Ts and soil water potential (Psis) on rs. To minimize the confounding effect of temperature, we analyzed the effect of Psis on rs during the summers of 1998-2000 when changes in Ts were slight. Soil respiration declined 25-50% in response to modest water stress (minimum Psis of -0.6 to -0.2 MPa), and between years, there was substantial variation in the relationship between rs and Psis. In the summer of 2000, 2-m2 plots were subjected to drought for 1 month and other plots were irrigated. The relationship between summertime rs and Psis in the experimental plots was similar to that estimated from the survey data obtained during the same summer. In late spring and early autumn of 2001, 2-m2 trenched and untrenched plots were subjected to drought or exposed to rainfall. It was dry in the early autumn and there was severe soil drying (Psis of -10 MPa in untrenched plots and -2 MPa in trenched plots). In spring, rs in untrenched plots responded more to modest water stress than rs in trenched plots, indicating that root respiration is more sensitive than microbial respiration to water stress at this time of year. The response to abiotic factors differed significantly between spring and autumn in untrenched plots but not in trenched plots, indicating that root activity was greater in early autumn than in late spring, and that roots acclimated to the sustained, severe water stress experienced before and during the autumn.
1998年至2001年期间,在一个香脂冷杉(Abies balsamea (L.) Mill.)生态系统中测量了土壤呼吸(rs)、土壤温度(Ts)和土壤容积含水量。根系和微生物呼吸的季节性变化以及非生物因素的协变混淆了Ts和土壤水势(Psis)对rs影响的解释。为了尽量减少温度的混杂效应,我们分析了1998 - 2000年夏季Ts变化较小时Psis对rs的影响。适度的水分胁迫(最低Psis为-0.6至-0.2 MPa)会使土壤呼吸下降25 - 50%,并且在不同年份之间,rs与Psis的关系存在很大差异。2000年夏季,对2平方米的样地进行了1个月的干旱处理,其他样地进行了灌溉。实验样地夏季rs与Psis之间的关系与同一夏季调查数据估计的关系相似。2001年春末和初秋,对2平方米的开沟和未开沟样地进行干旱处理或使其暴露于降雨中。初秋天气干燥,土壤严重干燥(未开沟样地的Psis为-10 MPa,开沟样地为-2 MPa)。春季,未开沟样地的rs对适度水分胁迫的响应比开沟样地的rs更明显,这表明在一年中的这个时候,根系呼吸比微生物呼吸对水分胁迫更敏感。未开沟样地对非生物因素的响应在春季和秋季之间存在显著差异,而开沟样地则没有,这表明初秋的根系活性大于春末,并且根系适应了秋季之前和期间经历的持续严重水分胁迫。