aspects of water resources and land use in the distrito ......pipiripau. decrease of baseflow...
TRANSCRIPT
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1Patrocinadopor
Funded by
IWASBrazilÁGUA-DF
Aspects of Water Resources and Land Use in the Distrito Federal
Carsten Lorz
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Jornal de Brasília 22.3.2011
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Fore
stC
erra
do T
ipic
oet
c.
Agric
ultu
re
urbanother
Land
use
Dramatic change of land use/land cover
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Pipiripau
Decrease of baseflow discharge
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Sediments
FRANZ C. ET AL. (2014) Environmental Earth Sciences, 72 (12) 4873-4890*LORZ C . ET AL. (2014) IWA Publications (ISBN 978-1-78040-489-9)OLIVEIRA V. ET AL. (2014) Environmental Earth Sciences (DOI 10.1007/s12665-014-3103-2)*FRANZ C. ET AL. (2014) Science of the Total Environment 466–467, 513–523*FRANZ C. ET AL. (2013) Science of the Total Environment 452–453, 411-420*FRANZ C. ET AL. (2012) Journal of Environmental Earth Sciences 65 (5), 1601-1611*
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
CharcoalKIA 41658
4405 ±25 BP
Charcoal KIA 41659
5285 ±40 BP
CharcoalKIA 41657
5954 ±40 BP
CharcoalKIA 41656
6470 ±70 BP
Sedimentation rates
14C (5285-4405): 0,05 cm a-1
14C (5954-5285): 0,13 cm a-1
14C (6470-5954): 0,03 cm a-1
Franz 2012
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Franz 2012
Site Sediment thickness[cm]
Sedimentation rate[cm yr-1]
period[yr]
Site 1
Site 2
Site 3
Site 4
* based on 137 Cs signature# based on alien materials
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015Brasilien
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015Brasilien
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
upperslope
Sediment Cascade
lower slope
urban areas
gullyerosion
alluvial system
alluvial system
lake
Eros
ion
Eros
ion/
Sedi
men
tatio
nSe
dim
enta
tion
Ret
entio
nR
eten
tion
Gen
erat
ion
Gen
erat
ion
R e
s i
d e
n c
e
t i m
e
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Franz et al. 2013
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Franz et al. 2013
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Land cover & contribution to alluvial sediments
Lago Paranoá BasinUrban 85 % / 34 % ⇒ 2.5Agric. 5 % / 8 % ⇒ 0.6 Natural 10 % / 58 % ⇒ 0.2
[%] Land use / [%] sediments = factor
Riacho Fundo BasinUrban 53 % / 38 % ⇒ 1.4Agric. 31 % / 47 % ⇒ 0.7 Natural 16 % / 12 % ⇒ 1.3
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Conclusions (1)o Sedimentation rates in modern times, i.e.
after 1960, are 10-100 times highero Sediments from urban, agricultural and
natural areas have distinct geochemicalfingerprints
o Fingerprinting method might help to quantifysources in frame of a sediment managementplan
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
SWAT Modelling
LORZ C. ET AL. (2014) IWA Publications (ISBN 978-1-78040-489-9)LIMA JEFW ET AL. (2013) Proceedings SWAT conference 2013, Toulouse, 10 pSTRAUCH M. ET AL. (2013) Journal of Environmental Management 127, 24-36STRAUCH M. ET AL. (2012) Journal of Hydrology 414-415, 413-424
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Conclusions (2)o Using a precipitation data ensemble leads to
more robust model resultso Multi-diverse crop rotations including irrigation
were found to be disadvantageous in terms of water availability by reducing base flow
o BMPs such as parallel terraces and small sediment basins (barraginhas) can lead to sediment load reductions of up to 40 % without affecting water yield
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Land use planning tool
LORZ C. ET AL. (2014) IWA Publications (ISBN 978-1-78040-489-9)KOSCHKE L ET AL. (2014) Ecological Processes, DOI 10.1186/2192-1709-3-2*LORZ C. ET AL. (2013) Journal of Environmental Management 127, S15-S23*
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Sediment retention
Runoff control
Agronomic
value
Nitr
ogen
fert
ilize
r
*
reference
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
landscape processes and function (LPF)
parameter reference
Sediment retention C factor (USLE) Morgan, 1995; Silva, 2007; Roose, 1976; Halbfaß & Grunewald, 2008; Lima & Lopez, 2009
Run off control CN value US SCS, 1972; USDA, 2004; Gonçalves, 2007; Franke, 1994/1995
Nitrogen loss control applied fertilizer [kg N ha-1 a-1]
FAO, 2010
Agronomic value yield [€ ha-1 a-1] IBGE, 2009
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Landnutzung spezifischSedimenteintrag [C-
Faktor der USLE]C-Faktor Standardisiert [0
bis 100]Agrarischer Wert [€/ha] nach IBGE7
Standardisiert [0 bis 100]
Wasserrückhalt [CN-Wert nach US SCS-Verfahren]8
Standardisiert [0 bis 100]
Gewässer-qualität [N
kg/ha]
Standardisiert [0 bis 100]
Acker, nicht spezifiziert
Acker, Sojabohnen, konventionell 0,20-0,501 0,35 35 503,96 7 72 69 7 6
Acker, Sojabohnen, no-tillage 0,172 2 0,172 17 503,96 7 64 54 0 0
Acker, Mais, konventionell
0,1720;2 0,40-0,90;3
0,02-0,90;1 >0,40 4 0,65 65 710,65 10 72 69 40 35
Acker, Mais, no-tillage 0,08-0104 0,09 9 710,65 10 64 54 0 0
Acker, Bohnen 0,30-0,401 0,35 35 978,78 14 72 69 11 10
Acker, Hirse 0,40-0,90;3 0,02-0,91 0,65 65 205,62 3 64 54 9 8
Acker, Weizen 0,10-0,40 1 0,25 25 1.010,36 15 64 54 9 8
Acker,Baumwolle0,50-0,70;3 0,40-
0,701 0,55 55 810,94 12 70 65 90 78
Acker, Kaffee0,10-0,30; 3 0,05; 1
0,219 20,219 22 1.226,75 18 66 57 115 100
Obst
Ananas, Avocado, Banane, Feige,
Guave, Mandarine, Mango, Maracuja, Orange, Papaya, Wassermelone,
Weintraube, Zitrone
Papaya: 0,21;1
Orangenplantagen: 0,21902
0,219 22 6.281,75 92 57 41 55 48
Gemüse
Annattostrauch, Kartoffel, Knoblauch,
Maniok, Reis, Süßkartoffel, Tomate, Zuckerrohr, Zwiebel
Süßkartoffel: 0,40-0,50;1 0,2-0,8;3
Maniok: 0,20-0,80;3
Zuckerrohr: 0,1743;2
0,13-0,40;1
Kartoffel: 0,1-0,51
0,5 50 6.847,91 100 70 65 57 50
Tierproduktion 0,1242 1 0,1242 12 59 44 0 0
Wiesen und Weiden 0,02-0,055 0,035 4 0 0 49 26 0 0
Grassteppe „Campo“ 0,01 1,3 0,01 1 0 0 89 100 0 0
Steppe „Cerrado“ 0,01 1,3 0,01 1 0 0 35 0 0 0Aufforstung 0,047 2 0,047 5 0 0 43 15 0 0Buschland 0,001 1 0,001 0 0 0 35 0 0 0
Naturnahe Wälder 0,001 1,3 0,001 0 0 0 55 37 0 0Verbrannte Fläche 0,160 6 0,16 16 0 0 74 72 0 0
vegetationslos 1 1,2,3 1 100 0 0 77 78 0 0
Siedlungsflächen 0,1242 1 0,1242 12 0 0 77 78 0 0Wasserflächen 0,14 1 0,14 14 0 0 -- -- 0 0
Sediment retention [C factor]Soy bean tillage 0.35 Soy bean no-tillage 0.17
Agronomic value [€ ha-1]Soy bean 704 Fruits 6.281
Runoff control [CN]Soy bean tillage 72 Soy bean no-tillage 64
N fertilizer [kg ha-1]Soy bean tillage 7 Corn tillage 40
Goldbach 2010
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Sediment retention
Runoff control
Agronomic
value
Land use [%]*
Nitr
ogen
fert
ilize
r
no tillage ⇒ tillage
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Water Resources and Land Use in DFPresentation at UFSCNovember 6th, 2015
Conclusions (3)o LdB is a land use planning support tool with
focus on sediments but other landscape functions or ecosystem services are integrated open to modification transparent & easy to handle, participation is easy spatially explicit ⇒ ZEE zoning
o LdB is an integrating approach helping to bridge the gap between “real” models and landscape planning