IP-W " ~ - ` - JUWEL - Forschungszentrum Jülich

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Schriften des <strong>Forschungszentrum</strong>s <strong>Jülich</strong> Reihe Umwelt/Environment Band/Volume 52
Page 1: P-W " ~ - ~ ` %I , 0 .; , ./ 1~ '`~
Page 5 and 6: Bibliographic information published
Page 8 and 9: 1 Introduction . . . . . . . . . .
Page 10: Introduction
Page 13 and 14: implemented in order to minimize th
Page 15 and 16: --- National border Cities h~ Water
Page 18 and 19: 2.1 The TRACE Model TRACE (Vereecke
Page 20 and 21: equal to h + z . Another special ty
Page 22 and 23: Y ö Ü 0 .8 ö 0 .6 - U 0 .4 0 .2
Page 24 and 25: No =Np +Ni (13) The overflowing buc
Page 26 and 27: lysimeter results for different soi
Page 28 and 29: 1 z 71.1 NW NE PArMOORE, SW / X / I
Page 30 and 31: 0,9 Deciduous forest (sandy soil) -
Page 32 and 33: 2.2.5 Deriving the groundwater rech
Page 34 and 35: Arranged MoLR-values according to s
Page 36 and 37: It is then verified for the remaini
Page 38 and 39: Fig . 7 summarizes the procedure in
Page 40: Data preparation and regionalizatio
Page 43 and 44: crops are corn, potatoes and oat .
Page 45 and 46: This relation was used to calculate
Page 47 and 48: The results of the PTFs are shown i
Page 49 and 50: The mean precipitation measured at
Page 51 and 52: 3.2.1 Climatic data bases All the c
Page 53 and 54:
--- National border ( . Waterbodies
Page 55 and 56:
National border _ . Waterbodies Cit
Page 57 and 58:
Tab . 7 : Landcover categories in t
Page 59 and 60:
TaE&Pere4ae dmebndcvrunmo$eCLCdassu
Page 61 and 62:
Groundwater level The groundwater n
Page 63 and 64:
Sites with a medium to deep depth t
Page 65 and 66:
The available field moisture capaci
Page 67 and 68:
The cMla~ Ns m mgh mrsmm|d«anc s o
Page 69 and 70:
-- National border Waterbodies " Ci
Page 71 and 72:
The sum of the available field capa
Page 73 and 74:
68 0Holocene 0Pleistocene 0Tertiary
Page 75 and 76:
National border Waterbodies Cities
Page 77 and 78:
Page 79 and 80:
The higher relief energy of the Rhe
Page 82:
Model results
Page 85 and 86:
Fig . 18 shows the results of this
Page 87 and 88:
Page 89 and 90:
Page 91 and 92:
4.2.2 Total runoff Fig . 21 shows t
Page 93 and 94:
Tab . 16 shows the statistical data
Page 95 and 96:
Page 97 and 98:
92 sn d R za 0 direct runoff level
Page 99 and 100:
Tab . 18 : Ranges and medians of th
Page 101 and 102:
In the consolidated rock regions of
Page 104 and 105:
5.1 Microscale The validation of wa
Page 106 and 107:
( In order to evaluate the model pe
Page 108 and 109:
0.4 0 .35 0.3 0 .25 0.2 0 .15 0.1 0
Page 110 and 111:
indicate that all relevant processe
Page 112 and 113:
possible determined by lysimeter ex
Page 114 and 115:
The vIdälon U me mo+ rs |s! wa p~r
Page 116 and 117:
leading to a lowering of the local
Page 118 and 119:
m -12 E 0 r- 2 E 2) 200 m r 0m m 3
Page 120 and 121:
GROWA and TRACE . For this purpose,
Page 122 and 123:
A slight improvement of the coeffic
Page 124 and 125:
The results of these investigations
Page 126:
Disaggregation of nutrient balances
Page 129 and 130:
ers to obtain information about are
Page 131 and 132:
component thus serves as a coordina
Page 133 and 134:
ating function not necessarily havi
Page 135 and 136:
included in an analysis as spatial
Page 137 and 138:
Tab . 23 : Classification quality a
Page 139 and 140:
--- National border Cities Map edit
Page 141 and 142:
On the assumption that each process
Page 143 and 144:
138 Aachen 6.4 Conclusion Dueren __
Page 146:
Summary
Page 149 and 150:
BK50, the digital hydro-geological
Page 152:
References
Page 155 and 156:
Doorenbos, J & Pruitt . W.O . (1977
Page 157 and 158:
Jahn, R (2002) : Erstellung eines h
Page 159 and 160:
RWE Power (2004) : http://www.rwepo
Page 162 and 163:
Schriften des Forschungszentrums J
Page 164 and 165:
Page 166 and 167:
Page 168 and 169:
Page 171:
Despite the fact that a clear water
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