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7.2 NANOPARTICLES AND ENVIRONMENT                                            FUNDAMENTALS

                                           photochemical
                                           reaction  + hv     monomer           nuclear
                                                               H O
                                           thermal OH, HO , RO ,
                                      H O            2   2      2        nuclear
                                       2   reaction         H SO 4
                                                             2
                                      SO 2                                      (H 2 SO 4 ) m (H 2 O) n
                                                   (gas phase)      homogeneous
                                      NO x                           nucleation
                                      HC
                                                           heterogeneous nucleation
                                                              (condensation)
                                                                           particle
                                          Characteristics function of aerosol f  condensation
                                   ∂f        ∂f                                particle
                                         =       migration, diffusion
                                   ∂t  total  ∂t  A
                                             ∂f
                                         +       chemical reaction
                                             ∂t  B
                                         +   ∂f
                                                 settling, deposition, washout, rainout
                                             ∂t  C
                                             ∂f
                                         +       condensation, coagulation, evaporation
                                             ∂t  D
                                             ∂f
                                         +       particle formation
                                             ∂t  E
                  Figure 7.2.3
                  Generation mechanisms of atmospheric nanoparticles and characteristics function.



                                   References                     Fig. 7.2.4 [1] is a conceptual figure showing colloid
                                                                 movement in soil strata. A is a heterogeneous layer com-
                  [1] C.A. Pope, J.M.  Thun, M.M. Namboodiri,  W.D.  posed of macropores formed in rotten roots close to the
                     Dockery, S.J. Evans, E.F. Speizer and W.C. Heath: Am.  ground surface. When rain falls, colloids move through
                     J. Respir. Crit. Care Med., 151, 669–674 (1995).  macropores saturated with water. B is a saturated
                  [2] M. Kasahara: J. Jpn. Soc. Air Pollut., 29(6), A100 (1994).
                  [3] M. Kasahara: J. Jpn. Soc. Air Pollut., 25(2), 115 (1990).


                  7.2.2 Ground water environments and nanoparticles
                  Particulate materials in water are present in the form of
                  colloids. These colloid particles are classified into inor-
                  ganic colloids. Examples of the former are oxides of alu-
                  minum, silicon and other substances, and typical
                  examples of the latter are substances such as humic acid
                  and fulvic acid. While the structure and molecular weight
                  of particles vary depending on the area of water, it is
                  known that what are usually present in water are com-
                  paratively small colloids (particles smaller than 500 nm).
                  The number concentration of colloid particles in ground
                  water, or a typical water area environment, ranges from
                                       3
                  10 11  to 10 20  (number/m ) and varies significantly
                  depending on the geochemical conditions of the aquifer.
                    It is known that in moving water, colloid particles
                  sometimes act as a medium in conjunction with water  Figure 7.2.4
                  and in some cases move faster than water.      Concept of colloid movements in soil strata.

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