欢迎访问《应用生态学报》官方网站,今天是 分享到:

应用生态学报 ›› 2002, Vol. ›› Issue (10): 1323-1338.

• 研究论文 • 上一篇    下一篇

开放系统中农作物对空气CO2浓度增加的响应

B. A. Kimball1, 朱建国2, 程磊2, K. Kobayashi3, M. Bindi4   

  1. 1. U.S.Water Conservation Laboratory, USDA, Agricultural Research Service Phoenix, Arizona, 85040, USA;
    2. 中国科学院南京土壤研究 所, 南京, 210008;
    3. National Institute of Agro-Environmental Sciences, Tsukuba, Ibaraki, 305-8604, Japan;
    4. Department of Agronomy and Land Management, University of Florence, 50144 Florence, Italy
  • 收稿日期:2002-07-08 修回日期:2002-08-03 出版日期:2002-10-15
  • 通讯作者: 朱建国,E-mail:jgzhu@issas.ac.cn.
  • 基金资助:
    中国科学院知识创新重要方向项目(KZCX2408);国家自然科学基金重大国际合作研究资助项目(40120140817).

B.A.Kimball1, ZHU Jianguo2, CHENG Lei2, K. Kobayashi3, M.Bindi4   

  1. 1. U.S.Water Conservation Laboratory, USDA, Agricultural Research Service Phoenix, Arizona, 85040, USA;
    2. Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008;
    3. National Institute of Agro-Environmental Sciences, Tsukuba, Ibaraki, 305-8604, Japan;
    4. Department of Agronomy and Land Management, University of Florence, 50144 Florence, Italy
  • Received:2002-07-08 Revised:2002-08-03 Online:2002-10-15

摘要: FACE试验(free-air CO2 enrichment)开展的10多年中,供试农作物主要有:C3禾本科作物小麦(Triticum aestivum L.)、多年生黑麦草(Lolium perenne)和水稻(Oryza sativa L.),C4禾本科类高粱(Sorghum bicolor(L.)Mench),C3豆科植物白三叶草(Trifolium repens),C3非禾本科块茎状作物马铃薯(Solanum tuberosum L.),以及多年生C3类木本作物棉花(Gossypium hirsutumL.)和葡萄(Vitis viniferaL.).本文系统整理和分析了以下各项参数的结果:光合作用、气孔导度、冠层温度、水分利用、水势、叶面积指数、根茎生物量累积、作物产量、辐射利用率、比叶面积、N含量、N收益、碳水化合物含量、物候变化、土壤微生物、土壤呼吸、痕量气体交换以及土壤碳固定.CO2浓度升高对农作物的影响作用主要表现在以下方面:(1)促进了植物光合作用、增加了其生物量累积;(2)显著提高C3作物产量,但对C4作物产量的影响很小;(3)降低了C3和C4作物气孔导度,非常显著地提高了所有作物的水分利用率;(4)对植物生长的促进作用在水分不足与水分充足时二者相当或前者大于后者;(5)对非豆科植物生长的促进作用要受到土壤低N水平限制,而对豆科植物则不受氮肥水平限制;(6)对根系生长的促进作用要大于地上部分;(7)对多年

关键词: CO2, 全球变化, 农作物生长, 产量, 水分, 氮, 碳固定, 开放系统

Abstract: Over the past decade, free-air CO2 enrichment (FACE) experiments have been conducted on several agricultural crops:wheat(Triticum aestivum L.), perennial ryegrass (Lolium perenne), and rice(Oryza sativa L.) which are C3 grasses; sorghum (Sorghum bicolor (L.) Möench), a C4 grass; white clover (Trifolium repens), a C3 legume; potato (Solanum tuberosum L.), a C3 forb with tuber storage; and cotton (Gossypium hirsutum L.) and grape (Vitis vinifera L.) which are C3 woody perennials. Using reports from these experiments, the relative responses of these crops was discussed with regard to photosynthesis, stomatal conductance, canopy temperature, water use, water potential, leaf area index, shoot and root biomass accumulation, agricultural yield, radiation use efficiency, specific leaf area, tissue nitrogen concentration, nitrogen yield, carbohydrate concentration, phenology, soil microbiology, soil respiration, trace gas emissions, and soil carbon sequestration.Generally, the magnitude of these responses varied with the functional type of plant and with the soil nitrogen and water status. As expected, the elevated CO2 increased photosynthesis and biomass production and yield substantially in C3 species, but little in C4, and it decreased stomatal conductance and transpiration in both C3 and C4 species and greatly improved water-use efficiency in all the crops. Growth stimulations were as large or larger under water-stress compared to well-watered conditions. Growth stimulations of non-legumes were reduced at low soil nitro-gen, whereas elevated CO2 strongly stimulated the growth of the clover legume both at ample and under low Nconditions. Roots were generally stimulated more than shoots. Woody perennials had larger growth responses to elevated CO2, while at the same time, their reductions in stomatal conductance were smaller. Tissue nitrogen concentrations went down while carbohydrate and some other carbon-based compounds went up due to elevated CO2, with leaves and foliage affected more than other organs. Phenology was accelerated slightly in most but not all species. Elevated CO2 affected some soil microbes greatly but not others, yet overall activity appears to be stimulated. Detection of statistically significant changes in soil organic carbon in any one study was impossible, yet combining results from several sites and years, it appears that elevated CO2 did increase sequestration of soil carbon.Whenever possible, comparisons were made between the FACEresults and those from prior chamber-based experiments reviewed in the literature. Over all the data and parameters considered in this review, there are only two parameters for which the FACE-and chamber-based data appear to be inconsistent. One is that elevated CO2 from FACEappears to reduce stomatal conductance about one and a half times more than observed in prior chamber experiments. Similarly, elevated CO2 appears to have stimulated root growth relatively more than shoot growth under FACEconditions compared to chamber conditions. Nevertheless, for the most part, the FACE-and chamber-based results have been consistent, which gives confidence that conclusions drawn from both types of data are accurate. However, the more realistic FACEenvironment and the larger plot size have enabled more extensive robust multidisciplinary data sets to be obtained under conditions representative of open fields in the future high-CO2 world.

中图分类号: