不同土壤温度下土壤水分胁迫对大豆幼苗净碳分配的影响

Botanical Gazette Pub Date : 1990-12-01 DOI:10.1086/337849
E. Mccoy, L. Boersma, M. Ekasingh
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引用次数: 12

摘要

不同土壤温度下水分胁迫对大豆净光合碳分配的影响[j]。[Merr.])采用区隔分析进行了调查。实验阶段采用经典的14C标记方法,植物在-0.04、- 0.25和-0.50 MPa的土壤水势下平衡;土壤温度分别为25℃和10℃,分区分析采用McCoy等人(1989)的方法。在两种土壤温度下,随着水分胁迫的增加,茎尖的碳固定速率一般随叶片伸长速率的增加而降低。然而,当中度水分胁迫导致叶片伸长率急剧下降时,碳固定率只有在严重水分胁迫水平下才会急剧下降。土壤温度降低降低了非水分胁迫处理的根和根瘤的碳固定化。这一关系与严重水分胁迫相反,土壤温度越低,根系和根瘤的碳固定化程度越高。显然,随着水分胁迫的增加,这些组织对生长和/或碳储量的需求增加,克服了低土壤温度的限制。在25℃土壤温度下,随着中度水分胁迫,碳库大小和向汇组织分配的碳量均增加,池大小的增加与中度水分胁迫下全株渗透调节一致。增加对汇的分配与碳转运过程受水分胁迫的影响比光合作用小一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Net Carbon Allocation in Soybean Seedlings as Influenced by Soil Water Stress at Two Soil Temperatures
The influence of water stress at two soil temperatures on allocation of net photoassimilated carbon in soybean (Glycine max [L.] Merr.) was investigated using compartmental analysis. The experimental phase employed classical 14C labeling methodology with plants equilibrated at soil water potentials of -0.04, -0 25 and -0.50 MPa; and soil temperatures of 25 and 10 C. Compartmental analysis followed that of McCoy et al. (1989). Carbon immobilization in the shoot apex generally followed leaf elongation rates with decreases in both parameters at increasing water stress at both soil temperatures. However, where moderate water stress resulted in dramatic declines in leaf elongation rates, carbon immobilization rates were sharply decreased only at severe water stress levels. Carbon immobilization was decreased in the roots and nodules of the nonwater stressed treatment by the lower soil temperature. This relation was reversed with severe water stress, and carbon immobilization in the roots and nodules was increased at the lower soil temperature. Apparently, the increased demand for growth and/or carbon storage in these tissues with increased water stress overcame the low soil temperature limitations. Both carbon pool sizes and the partitioning of carbon to the sink tissues increased with moderate water stress at 25 C soil temperature Increased pool sizes were consistent with whole plant osmotic adjustment at moderate water stress. Increased partitioning to the sinks was consistent with carbon translocation processes being less severely influenced by water stress than is photosynthesis.
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