首页> 美国卫生研究院文献>Frontiers in Physiology >The Thermodynamic Flow-Force Interpretation of Root Nutrient Uptake Kinetics: A Powerful Formalism for Agronomic and Phytoplanktonic Models
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The Thermodynamic Flow-Force Interpretation of Root Nutrient Uptake Kinetics: A Powerful Formalism for Agronomic and Phytoplanktonic Models

机译:根营养吸收动力学的热力学流动力解释:农学和浮游植物模型的强大形式主义

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摘要

The ion influx isotherms obtained by measuring unidirectional influx across root membranes with radioactive or stable tracers are mostly interpreted by enzyme-substrate-like modeling. However, recent analyses from ion transporter mutants clearly demonstrate the inadequacy of the conventional interpretation of ion isotherms. Many genetically distinct carriers are involved in the root catalytic function. Parameters Vmax and Km deduced from this interpretation cannot therefore be regarded as microscopic parameters of a single transporter, but are instead macroscopic parameters (Vmapp and Kmapp, apparent maximum velocity and affinity constant) that depend on weighted activities of multiple transporters along the root. The flow-force interpretation based on the thermodynamic principle of irreversible processes is an alternative macroscopic modeling approach for ion influx isotherms in which macroscopic parameters Lj (overall conductance of the root system for the substrate j) and πj (thermodynamic parameter when Jj = 0) have a straightforward meaning with respect to the biological sample studied. They characterize the efficiency of the entire root catalytic structure without deducing molecular characteristics. Here we present the basic principles of this theory and how its use can be tested and improved by changing root pre- and post-wash procedures before influx measurements in order to come as close as possible to equilibrium conditions. In addition, the constant values of Vm and Km in the Michaelis-Menten (MM) formalism of enzyme-substrate interpretation do not reflect variations in response to temperature, nutrient status or nutrient regimes. The linear formalism of the flow-force approach, which integrates temperature effect on nutrient uptake, could usefully replace MM formalism in the 1-3-dimension models of plants and phytoplankton. This formalism offers a simplification of parametrization to help find more realistic analytical expressions and numerical solution for root nutrient uptake.
机译:通过使用放射性或稳定示踪剂测量跨根膜的单向流入量而获得的离子流入等温线大多由酶-底物样模型解释。但是,最近对离子转运蛋白突变体的分析清楚地表明,对离子等温线的常规解释是不够的。许多遗传上不同的载体参与了根的催化功能。因此,从这种解释推导出的参数Vmax和Km不能被视为单个转运蛋白的微观参数,而是宏观参数(V m a p p 和K m a p p ,表观最大速度和亲和常数)取决于沿根部多个转运蛋白的加权活性。基于不可逆过程的热力学原理的流动力解释是一种用于离子流等温线的替代宏观建模方法,其中宏观参数Lj(基质j的根系的总电导)和πj(Jj = 0时的热力学参数)对于所研究的生物样品具有直接的含义。它们表征了整个根催化结构的效率,而没有推断分子特征。在这里,我们介绍了该理论的基本原理,以及如何通过在流入量测量之前更改根的清洗前和清洗后程序来测试和改进其使用,以尽可能接近平衡条件。另外,酶-底物解释的米利斯-门滕(MM)形式中的Vm和Km恒定值不能反映对温度,养分状况或养分状况的响应变化。流力法的线性形式,结合了温度对养分吸收的影响,可以有效地替代植物和浮游植物的1-3维模型中的MM形式。这种形式主义简化了参数化,以帮助找到更现实的分析表达式和根营养素吸收的数值解。

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