scholarly journals Laundry Detergency of Solid Non-Particulate Soil Using Microemulsion-Based Formulation

2018 ◽  
Vol 67 (2) ◽  
pp. 187-198 ◽  
Author(s):  
Jarussri Chanwattanakit ◽  
Sumaeth Chavadej
Keyword(s):  
1969 ◽  
Vol 46 (10) ◽  
pp. 537-543 ◽  
Author(s):  
B. E. Gordon ◽  
W. T. Shebs
Keyword(s):  

2015 ◽  
Vol 85 ◽  
pp. 22-30 ◽  
Author(s):  
Sebastián R. Mazzilli ◽  
Armen R. Kemanian ◽  
Oswaldo R. Ernst ◽  
Robert B. Jackson ◽  
Gervasio Piñeiro

1986 ◽  
Vol 35 (7) ◽  
pp. 538-542
Author(s):  
Chikako TAMURA ◽  
Masako SATO ◽  
Motoi MINAGAWA
Keyword(s):  

1976 ◽  
Vol 46 (6) ◽  
pp. 459-462 ◽  
Author(s):  
Hans Schott

The simplest expressions for the rate of removal of particulate soil from fabrics, including those for first-order kinetics, are described. Two factors militate against obtaining proportionality constants between a time function and a residual soil function which remain constant for long washing times, namely: redeposition, and heterogeneities in soil and fabric. Soil redeposition tends to lower the observed soil-removal rate. This effect can be eliminated by suitable experimental procedures. However, the inhomogeneities inherent in fabrics (fiber surface irregularities, variation in spaces between fibers and yarns) cause them to have sorption sites with a broad range of soil binding strengths. Variations in the size and shape of particles on artificial test fabrics and, for natural soil, in chemical composition as well, cause the particles to adhere to fabric substrates with bonds of different strengths. These heterogeneities produce a broad range of specific soil-removal rates whose values depend on the energies of adhesion of the particle-fabric complex. The most loosely held soil, with the highest removal rate constants, is washed off early so that the soil remaining on the fabric becomes progressively richer in the most tightly bound soil, with the smallest removal rate constants. Hence the average or observed rate constant for soil removal decreases during the washing process.


Author(s):  
Garrison Sposito

In Section 3.4, the cation exchange capacity, or CEC, of particulate soil humus is defined as the maximum number of moles of proton charge per kilogram that can be desorbed by a metal cation under prescribed conditions. Thus, CEC for particulate humus is equal to the maximum absolute value of the negative net proton charge. Operationally, this maximum value is measured typically as the surface excess of Ba2+ adsorbed by humus at pH 8.2 (Eq. 3.5). Extending this concept to soils, one can define the CEC as the maximum number of moles of readily exchangeablemetal cation charge per unit mass of dry soil that can be extracted under prescribed conditions. In this more general context, CEC refers to metal cations that adsorb on soil particles in either outer sphere surface complexes or the diffuse ion swarm (Fig. 7.2). In alkaline soils, the common readily exchangeable cations are Ca2+, Mg2+, Na+, and K+, whereas in acidic soils, this group expands to include Al3+, and its complexes AlOH2+, Al(OH)2+, and AlSO+4. Following the operational paradigm for soil humus, one concludes that the measurement of soil CEC involves not only the desorption of protons, but also the replacement of the population of readily exchangeable adsorbed metal cations at a selected pH value (usually pH 7–8) by a chosen cation. Laboratory procedures for measuring CEC are described in Methods of Soil Analysis, listed in For Further Reading at the end of this chapter. In alkaline soils, the replacing cation chosen is often Na+ or Ca2+, whereas in acidic soils and for soil humus, the replacing cation of choice is Ba2+. These cations, in turn, are typically displaced from soil particle surfaces by Mg2+ to measure the surface excess. A conceptual definition of CEC can be developed in terms of the surface charge balance concepts introduced in Chapter 7. Consider first a soil in which a net positive surface excess of anions does not occur, such as the Mollisol example discussed in Section 8.1. In this case, the only adsorbed ions are Ca2+ and Cl-. The CEC of this soil may be defined by a special case of the charge-balance condition in Eq. 7.3a: ∆qex (max) ≡ CEC


2020 ◽  
Vol 108 ◽  
pp. 144-153
Author(s):  
Bianca Carreiro Cerri ◽  
Laíze Matos Borelli ◽  
Ingrid Martins Stelutti ◽  
Marcio Roberto Soares ◽  
Mariana Altenhofen da Silva

1965 ◽  
Vol 35 (5) ◽  
pp. 474-476 ◽  
Author(s):  
Brant A. Short

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