1) Nonequili brium sorption-desorption
非平衡吸附解吸
2) non-equilibrium adsorption/desorption
非平衡吸附/解吸
3) nonequilibrium sorption
非平衡吸附
1.
Influence on radionuclide migration by nonequilibrium sorption and identification of rate coefficient;
非平衡吸附对核素迁移的影响及平衡速率参数的确定
4) non-equilibrium adsorption
非平衡吸附
1.
A fuel cell vehicle air-conditioning system which is driven by waste heat employs activated carbon-methanol as refrigerant This paper is about the system simulation study solved by numerical method which based on the theory of non-equilibrium adsorption.
本文基于非平衡吸附理论,对冷却水流量队该系统性能的影响进行了数值计算和仿真研究。
2.
On the basis of the non-equilibrium adsorption model,the dynamic behavior of COP and SCP along with the time are calculated considering the temperature variation of heating fluid.
以非平衡吸附模型为基础,计算了加热流体温度变化时,系统的性能系数COP以及单位质量吸附剂制冷功率SCP随时间的变化,结果表明加热流体温度变化对系统COP和SCP值有很大影响,并且影响相对滞后于加热流体温度的变化。
3.
On the basis of the Linear Driving Force non-equilibrium adsorption model,the perfor- mance of composite zeolite/foam aluminum-water adsorption refrigeration are calculated at different thicknesses and cycle time.
基于线性驱动力(LDF)非平衡吸附模型,计算了不同吸附层厚度、不同循环周期沸石分子筛/泡沫铝复合吸附剂-水的基本循环吸附制冷性能。
5) non-equilibrium sorption
非平衡吸附
1.
Based on the fractal geometry and non-equilibrium sorption model of coalbed methane,the pseudo-steady mathematical models with well-bore storage and skin effects in fractal coalbed methane reservoir are presented when the constant flow rate is specified at the well-bore in infinitely large reservoir and bounded reservoir.
基于分形几何学和煤层气的拟稳态非平衡吸附动力学模型,建立了考虑井储和表皮效应的分形介质煤层气流动数学模型。
6) equilibrium/nonequilibrium two-site absorption-desorption
平衡/非平衡双点吸附解吸
1.
Considering the environment behaviors of contaminant in soil,such as diffusion,equilibrium/nonequilibrium two-site absorption-desorption and microbiological degradation,the kinetic model of the contaminants transport in soil is established;and its finite difference equation is given.
在考虑对流弥散、平衡/非平衡双点吸附解吸、微生物降解等情况下,建立了土壤环境中有机污染物迁移转化的动力学模型,并给出了有限差分解。
补充资料：土壤磷素吸附和解吸作用
土壤磷素吸附和解吸作用
adsorption and desorption of phosphorus in soil
磷与一OH基或一0H2其过程如下: (1)HZPO不和0H2进行配位交换而被专性吸附。交换即: OH] \/l M} /\lo/0H2曰\OH \/+H:PO一se/\0H2」 O H 十一﹁|l||习OH/\ 《)-P-心 /\OH OHOH M\\/\ O M/\ 0H:」(2)或者HZPO不和OH一交换，即Ho/ M \+HZPO不—一|一| HH/00\/ M/\/ 00H2 片 O 十刁|lwe|10H2\/\ (卜一P-城〕 /\OH OH OH一 /M \ 0H2一 \/ 0 过程(l)并不伴随着溶液的pH值改变，过程(2)可使溶液的pH值上升. 上述两过程的产物，随着时间的延续，都可以变为环状结构: OH+HZO;二二二已 OH一/\ OH:一 MM\/\/ 0+ZH:0/\/\ 0H21，，土城麟素吸附和解吸作用(adsorp‘on anddesorption of Phosphorus in 5011)土壤溶液中的碑酸离子被土城固相所吸持，谓之吸附。其逆向反应谓之解吸.吸附和解吸开始时都是发生在土壤固、液相的界面上.吸附作用可以发生在具有不变电荷土粒的表面(如结晶态的粘土矿物)，也可以发生在可变电荷的土粒表面(如铁铝氧化物、土壤有机质和方解石等物质)上。 碑素吸附土城对碑酸离子的吸附，分为物理吸附(非专性吸附)和化学吸附(专性吸附). 物理吸附当土城溶液的pH值低于土壤吸附剂的等电点时，吸附剂上的一OH墓被质子化: Me一OH+H+一Me一0H2+而后带正电荷的表面因静电引力吸引带负电的磷酸离子。
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