Gnaiger E, Bitterlich G
Institute for Marine Environmental Research, Prospect Place, The Hoe, PL 1 3DH, Plymouth, England.
Institut für Zoologie, Abteilung Zoophysiologie, Universität Innsbruck, Peter-Mayr-Str. 1A, A-6020, Innsbruck, Austria.
Oecologia. 1984 Jun;62(3):289-298. doi: 10.1007/BF00384259.
Carbohydrate, lipid, and protein compositions are stoichiometrically related to organic CHN (carbon, hydrogen, nitrogen) contents. Elemental CHN analyses of total biomass and ash, therefore, provide a basis for the calculation of proximate biochemical composition and bomb caloric value. The classical nitrogen to protein conversion factor (6.25) should be replaced by 5.8±0.13. A linear relation exists between the mass fraction of non-protein carbon and the carbohydrate and lipid content. Residual water in dry organic matter can be estimated with the additional information derived from hydrogen measurements.The stoichiometric CHN method and direct biochemical analysis agreed within 10% of ash-free dry biomass (for muscle, liver and fat tissue of silver carp; gut contents composed of detritus and algae; commercial fish food). The detrital material, however, had to be corrected for non-protein nitrogen.A linear relationship between bomb caloric value and organic carbon fractions was derived on the basis of thermodynamic and stoichiometric principles, in agreement with experimental data published for bacteria, algae, protozoa and invertebrates. The highly automatic stoichiometric CHN method for the separation of nutrient contents in biomass extends existing ecophysiological concepts for the construction of balanced carbon and nitrogen, as well as biochemical and energy budgets.
碳水化合物、脂质和蛋白质组成在化学计量上与有机CHN(碳、氢、氮)含量相关。因此,对总生物量和灰分进行元素CHN分析,为计算近似生化组成和弹式热量值提供了基础。经典的氮与蛋白质换算因子(6.25)应替换为5.8±0.13。非蛋白质碳的质量分数与碳水化合物和脂质含量之间存在线性关系。利用氢测量得到的额外信息,可以估算干有机物质中的残留水分。化学计量CHN方法与直接生化分析在无灰干生物量的10%范围内一致(对于鲢鱼的肌肉、肝脏和脂肪组织;由碎屑和藻类组成的肠道内容物;商业鱼食)。然而,碎屑物质必须校正非蛋白质氮。基于热力学和化学计量原理,得出了弹式热量值与有机碳分数之间的线性关系,这与已发表的关于细菌、藻类、原生动物和无脊椎动物的实验数据一致。用于分离生物量中营养成分的高度自动化化学计量CHN方法扩展了现有的生态生理学概念,用于构建平衡的碳和氮以及生化和能量预算。