w. ripl : 1 control of watercycle- and matter- flow by vegetation, approaches for a sustainable...
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W. Ripl : 1
Control of Watercycle- and matter-flow by Vegetation, approaches for
a sustainable Ressourcemanagement
W. Ripl
W. Ripl
2
Attenuation of an energy-pulse to the mean
So urc e : Hild m a nn 1993 Einlk1e .c d r, 26.9.94
te m p e ra ture
04 2
34
tim e
m e a n
m e a sure d te m p e ra ture
e ne rg y p ulsee .g . sune ne rg y
a tte nua tio nb y e .g . e va p o tra nsp ira tio n,c o nd e nsa tio n
d e via tio n o f m e a sure dte m p e ra ture fro m m e a n
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3
Structures and distributes processes by means of the dynamic Structures and distributes processes by means of the dynamic medium water in landscape medium water in landscape
It controlles the atmosphere with respect to its process It controlles the atmosphere with respect to its process dynamics,dynamics,composition und distributioncomposition und distribution
It controlles mechanical and chemical processes close to the soil It controlles mechanical and chemical processes close to the soil surface and distributes thereby organisms, it eliminates surface and distributes thereby organisms, it eliminates randomness, minimises material flows, and increases sustainable randomness, minimises material flows, and increases sustainable developmentdevelopment
It controlles temperature- and moisture patterns in space and It controlles temperature- and moisture patterns in space and time as a niche for all organismstime as a niche for all organisms
Nature as a dynamic energy- dissipative process
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Dissipative Ecological Unit (DEU)
ZKS4_a.cdr, 28.06.00
process contro lm atter cycle
water as transport, reaction and cooling agent
detritus
destruents consum ers
producers
energy
Source: R ip l & H ildm ann 1993
W. Ripl
6
BO 1
PB
BO 2
AT1
AT2
SB1
SB2
SA1
K-D
Wo
lter,
TU B
erli
n, F
ac
hge
bie
t Lim
nolo
gie
. Dig
erf_
1.c
dr,
26.0
1.00
SA2re c .
0 00 0,5 0,5150 5010050 0
8.000
6.000
4.000
2.000
100
years b.p.
zoneloss on ignition
g/m2 year g/m2 year g/m2 year mg/m2 year mg/m2 year
10.000
total P extr. Ca extr. Mg extr. K
Postglacial development of Lake Trummen (Sweden). Yearly deposition according to G. Digerfeldt (1972)
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Efficiency and selfoptimization in nature (ETR-concept)
Dissipative structures are the optimized materialized answers to energetic interaction problems far from thermodynamic equilibrium
The efficiency criteria (closed localized material cycles related to irreversible linear material flow) determines sustainability of dissipative structures
Periodically moving water in nature, metabolizing cells, reproducing organisms, coenotic structures competing for sustainability and selfoptimizing ecosystems are dissipative structures in different fractal organization levels
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Thesis 1
Nature is under stable conditions with respect to space and pulsed energy a recursive selforganisation process,
a steady development of sustainable dissipative structures such as organisms in interaction with their environment is the result.
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Thesis 2
Process distribution and -coupling in space and time determines the “irreversible” material flows to the sea and thereby sustainability and the ageing of the landscape
W. Ripl
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Thesis 3
Material flows were dramatically increased by men induced interference with the energy flow, the watercycle and the vegetation.
Material flows in nature consist of chargeflows in
rivers and groundewater, emissions, immissions and erosion
W. Ripl
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Thesis 4
The quality of the necessary functions of nature can be estimated by the spatial distribution of evaporable water in the landscape observed in the temperature distribution at the land surface.
The quality of ecological functions can be measured by satellite imagery on the one hand, on the other hand by the distribution of runoff and the material flow from the catchments measured as waterflow and irreversible charge flow.
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Thesis 5
The vegetation cover in feedback with the watercycle is the most important energy processor in the landscape
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Theoretical basis for thermal efficiency
m ean tem perature
increasing efficiency = minim al temperature deviation
- temperature deviation
decreasing efficiency = maximal tem perature deviation
m ean tem perature
wkgd_T, 14.9.95Source: m odified from H ildm ann 1993
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Irreversible matter losses by precipitation and run-off in different landscape types
K-D W olter, TUB - L im nologie; Transp_1.cdr, 11.12.00Source: R ip l 1995
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Development and Desertification of Landscape after glaciation had ceased
Water cycle, matter budget and temperature balance
h i s t o r 3 a . c d r 2 0 0 1 0 8 1 0 , C h r i s t i a n H i l d m a n n
2
°C
t
4
°C
t
6
°C
t
5
°C
t
3
°C
t
1
°C
t
W ide o pen wa ter cycle sho rta fter g la cia tio n
Sho rtcircu ited wa tercyclelo w p ro ba b ility fo r successio n
W a tercycle destro yedso il dep leted o f nutrients a nd m inera ls
W a tercycle o pened up ; m a tter lo sses; retentio n o f m a tter still in wetla nds M a teria l lo sses m a xim ized
Structurizing o f la ndsca pe
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ETR an ecological concept based on the energetics of water
Water in interaction with solid surface leads to sorting processes according to energetic dissipative properties (particle size, dissolution equilibria)
stagnant water leads to conservation of structures (achievement of equilibrium)
high and random water dynamics at liquid-solid interfaces lead to erosion of structures (increased mechanical and chemical interactions)
optimized dissipative structures are dynamic metabolizing structures at lowest energy flow density
W. Ripl
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The dissipative water cycle
g ro und wa te rg ro und wa te r
Ne um ünste ra g ric ulture
fo re stry
a g ric ulturefo re stry Ne um ünste r
ve g e ta tio n,susta ina b lea g ric ulture
a nd fo re stry
ve g e ta tio n,susta ina b lea g ric ulture
a nd fo re stry
ve g e ta tio n,susta ina b lea g ric ulture
a nd fo re stry
Ne um ünste rHa m b urg Ne um ünste rHa m b urg
Ha m b urg Kie lNe um ünste r Ha m b urg Kie lNe um ünste r
broa d open wa ter c yc le short c irc uit wa ter c yc le
re g io na lsc a le
e .g .c a tc h-m e nta re aStö r
lo c a lsc a le
e .g .Ne u-
m ünste r
na tio n-wid esc a le
e .g .No rth
G e rm a ny
Hild m a nn, FG Lim no lo g ie 9/94Wa kre i2e .c d r, 15.9.94
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Indicators for sustainable and non-sustainable water cycles and landscapes
0.3
0.6
0.9
1.2
1.5
0
0.3
0.6
0.9
1.2
1.5
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J F M A M J J A S O N
30
25
20
15
10
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-5
30
25
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10
5
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-5D
J F M A M J J A S O N D J F M A M J J A S O N D
J F M A M J J A S O N D
J F M A M J J A S O N D
J F M A M J J A S O N D
Lo_pr_1e.cdr, 94, 05.07.00
soil w ater tab le
soil w ater tab le
discharge [l/m ²/m onth]
tim e
tim e tim e tim e
tem perature so il surface
Natural ecosystem
D isturbed ecosystem
m inera liza tion zone
m inera liza tion zonedischarge
tem perature so il surface
losses
losses
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Climatic function dry field – wetland ( Pokorny 2001)
HEAT FLUX5 - 10 %
DRAINED FIELD LAKE, M EADO W, FO REST,LANDSC APE SATURATED WITH WATER
REFLEC TIO N5 - 15 %
REFLEC TIO N5 - 10 %
HEAT FLUX
5 - 10 %
HEAT
60 - 70 %
EVAPO TRANSPIRATIO N
70 - 80 %
DAILY INPUT O F SO LAR ENERG Y6 kWh.m
m a x e ne rg y flux800 - 1000 W.m
-2
-2
EVAPO TRANSPIRATIO N10 - 20 %
HEAT5 - 10 %
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Present environmental politics: regulation by threshold values
Gre
nzw
erts
teue
rung
Ad m in_ 1.c d r, 18.11.96Wo lte r & Rip l unp ub l.
a irwa te r
fixa
tion
of t
hre
sho
ld v
alu
es
sec toria l view
rea lity
dec ision m a king
le g isla tio n
le g isla tio n
so il
regula tion by lega l lim itsnot spa c e a nd tim e a d justed
m onitoring long
fe
ed
ba
ck,
ine
ffe
ctiv
eg
ap
be
twe
en
de
cis
ion
ma
king
and
re
alit
y
higha dm inistra tiveeffort
EU
fa rm e r a nd fo re st m a na g e r
m unic ip a litie s
c o untrie s
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29
Future target related regulation (holistic approach)
KD W olter, TU Berlin - L im nolog ie , Adm in_2.cdr, 06.02.01
highresponsib ility
W olter & R ip l unpubl.
air
w ater
functionalunderstanding
holistic viewpatternrecognition
fixing ofboundary conditions
soil
target-regulation towards sustainability,space and time related
areal m anager
leg islation, adm in istration
short, efficientfeed back
lowadministrativeeffort
decision makingnear reality
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What are Natures ecological services for a sustainable society?
The dissipative water cycle, evaporation and precipitation and its thermostatic function in the catchments
The atmosphere in its composition, its distribution and its dynamics
Soil fertility at dynamic conditions. Soil as the dynamic interface between vegetation and the minerogenic substrate under the local water-cycle conditions
The selforganizing plant cover as the efficient protector of habitat stability