Page 414 - Soil and water contamination, 2nd edition
P. 414

Answers to exercises                                                  401

                   c.   Calculate the cumulative total erosion and the transport capacity at the beginning and
                      end of each section.
                      Section     Slope length   Cumulative total erosion  Transport capacity
                                                     -1
                                  (m)            (kg m  y )             (kg m  y )
                                                                            -1
                                                                              -1
                                                       -1
                      1             0             0                      0
                                   50            9.6                    11.8
                      2            50            9.6                    32.2
                                  100            29.0                   54.1
                      3           100            29.0                    9.5
                                  150            34.8                   12.9
                        The cumulative total erosion does not exceed the transport capacity until the end of
                      section 2 (100 m from the divide). At the beginning of section 3 the transport capacity is
                      exceeded. It is here that the excess sediment is deposited.


                   CHAPTER 13


                   1. a.  C(t) = C  e -kt
                               0

                      b.  C(t) = C  + (C  - C ) e -kt
                               eq   0   eq
                   3.  a.  0.05 mg l -1
                      b.  0.086 mg l -1
                      c.   uptake of NH4 and/or NO3 by algae or aquatic macrophytes (sink); atmospheric
                         deposition (source); ammonia volatilisation (sink); adsorption of NH4 by suspended
                         solids (sink); decomposition of DOM or POM in the water column (source).
                   4.  a.   The concentration of o-xylene in this particular equation; the substrate concentration
                         in general.
                      b.  The analytical solution of the differential equation is
                                 S 0
                         1000 ln        S 0  S( t)    45 t
                                S( t)
                         The graph can be drawn to solve t for different values of S(t):














                      c.  approximately 100 days











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        Soil and Water.indd   413                                                           10/1/2013   6:47:54 PM
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