[1]张富仓,张一平,康绍忠.土壤水分运移的能垒分析[J].水土保持研究,1996,3(03):87-92.
Zhang Fucang,Zhang Yiping,Kang Shaozhong.An Analysis of Energy Barrier of Soil Water Movement[J].Research of Soil and Water Conservation,1996,3(03):87-92.
点击复制
《水土保持研究》[ISSN:1005-3409/CN:61-1272/P]
卷:
3
期数:
1996年03期
页码:
87-92
栏目:
出版日期:
1900-01-01
- Title:
-
An Analysis of Energy Barrier of Soil Water Movement
- 作者:
-
张富仓, 张一平, 康绍忠
-
西北农业大学, 陕西, 杨陵, 712100
- Author(s):
-
Zhang Fucang, Zhang Yiping, Kang Shaozhong
-
Narthwestern Agricultural University, Yangling, Shanxi, 712100
-
- 关键词:
-
活化能; 能垒; 土壤水流
- Keywords:
-
activation energy; energy barrier; soil water movement
- 摘要:
-
活化能是化学动力学中一个重要概念,当应用于土壤水流过程时,是指水流过程中需要克服的能垒(energybarrio).土坡水的表观或平均活化能是耗费在一个水分子越过两个流线准平衡位置势能垒所需能量,此能垒是速率限制因子,可由Arrhenius方程式计算.实验对陕西省四种典型土壤不同水流过程中活化能进行了测定计算,提出了“土壤水渗透活化能”,“渗吸活化能”,“扩散活化能”及“蒸发活化能”等概念.且此四种活化能均呈质地较粘重的土壤大于质地较轻的土坡,同一质地土壤其水分运移形式不同,活化能大小不同.“蒸发活化能”
- Abstract:
-
The activation energy is an important concept in thefield of chemical kinetics.Means a potEntial energy barrier which need to be overcome in soil water flow process.The apparent or average activation energies for soil water is the energy expended by a molecule in surmounting a potential energy barrier between two quasi-equlibrium positions along the line of flow,and it is factor of rate-limiting and can be calculated by Arrhenius equation.The activation ehergies are calculated from the experimental measurements for the four kinds of soils of Shannxi province at different soil water flow processes.This paper prcpound the idea of "Permeability Activation Energy","Infiltration Activation.Energy","Diffusion Activation Energy" and "Evaporation Activation Energy",and the value of four kinds of activation energies show that the heavy texture soils is higher more than light texture soils,for the same texture soils,the value of activation energy is depended on the soil water movement way,the activation energy of evaporation is much greater than the others kinds of activation energy.
参考文献/References:
[1] Anderson.D.M.,A.Linville.,and G.Sposito.,Temperature Fluctuations at a wetting front:Ⅱ.Apparent activation energies for water movement in the liquid and vapor phases.Soil Sci.Soc.Am.Proc.,1963.27:610-613
[2] Taylor.S.A.,(华孟等译).物理的土壤学,北京:农业出版社,1983
[3] Gardner.W.R.,Diffusivity of soil water during sorption as affected by temperature.Soil Sci.Soc.Am.Proc.,1959,23:406-408
[4] Jackson.R.D.,Temperature and soil-water diffusivity relations.Soil.Soc.Am.Proc.,1963,27:363-366
[5] Wiegand.G.E.,and S.A.Taylor.,Temperature depression and temperature distribution in dryng soil columns.Soil Sci.,1962,94:75-79
[6] 李开元,李玉山.黄土高原土壤在不同给水条件下的蒸发性能.干旱地区农业研究,1991,(3):77-83
更新日期/Last Update:
1900-01-01