{"title":"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","authors":"E. Mccoy, L. Boersma, M. Ekasingh","doi":"10.1086/337849","DOIUrl":null,"url":null,"abstract":"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.","PeriodicalId":9213,"journal":{"name":"Botanical Gazette","volume":"151 1","pages":"497 - 505"},"PeriodicalIF":0.0000,"publicationDate":"1990-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"12","resultStr":"{\"title\":\"Net Carbon Allocation in Soybean Seedlings as Influenced by Soil Water Stress at Two Soil Temperatures\",\"authors\":\"E. Mccoy, L. Boersma, M. Ekasingh\",\"doi\":\"10.1086/337849\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"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.\",\"PeriodicalId\":9213,\"journal\":{\"name\":\"Botanical Gazette\",\"volume\":\"151 1\",\"pages\":\"497 - 505\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1990-12-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"12\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Botanical Gazette\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1086/337849\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Botanical Gazette","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1086/337849","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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.