Download - Paolo Benettin

Transcript
Page 1: Paolo Benettin

On the Integrated Response of Catchments: benchmark applications using chloride and isotopic tracers

Paolo Benettin

Workshop on coupled hydrological modling Padova | 23 โ€“ 24 April 2015

Page 2: Paolo Benettin

age T

๐’‘๐‘ธ(๐‘ป, ๐’•)

Distribution of water parcels

time

๐ถ ๐‘ก = ๐‘ ๐‘‡ ๐’‘๐‘ธ ๐‘ป, ๐’• ๐‘‘๐‘‡

โˆž

0

fundamental link between water age and water quality

spatially-integrated approach

2

Page 3: Paolo Benettin

NO FERTILIZATION

Measurements from the Hupsel Brook Catchment, NL

1 โ€“ slow transport response

TTDs and transport

NL

outlet

2 โ€“ fast โ€˜reactivityโ€™ during storms

CHLORIDE concentration measurements

3

Page 4: Paolo Benettin

โ€ข fast calibration

โ€ข easy exploration of the parameter space

spatially-integrated approach

simplification of the system, no physically-based

descriptions

โ€˜softโ€™ models that capture the emergent transport

processes

suitable for hydrologic TRANSPORT and TTDs

effective integration of spatial complexity

4

Page 5: Paolo Benettin

integrated catchment response

from McDonnell et al., 2010, HP

realistic distributions ideal distributions

๐’‘๐‘ธ(๐‘ป, ๐’•)

smooth, easy to parameterize

irregular, time-variant

5

Page 6: Paolo Benettin

๐œ• [๐‘† ๐‘ก ๐’‘๐‘บ ๐‘‡, ๐‘ก ]

๐œ•๐‘ก+๐œ•[๐‘† ๐‘ก ๐’‘๐‘บ ๐‘‡, ๐‘ก ]

๐œ•๐‘‡= โˆ’๐‘„ ๐‘ก ๐Ž(๐‘‡, ๐‘ก) ๐’‘๐‘บ(๐‘‡, ๐‘ก)

Age Master Equation (after Botter et al., GRL, 2011):

younger water

๐Ž (๐‘‡, ๐‘ก)

1

older water

๐’‘๐‘บ(๐‘‡, ๐‘ก)

age tracking at catchment scale

age distribution of the water storage

StorAge Selection (SAS) functions

age T

RS

6

Page 7: Paolo Benettin

Random sampling: ๐‘๐‘„(๐‘‡, ๐‘ก) = ๐‘๐‘†(๐‘‡, ๐‘ก)

โˆž S(t)

Q(t) Q(t)

๐ถ๐‘„ ๐‘ก = ๐ถ๐‘† ๐‘‡โˆž

0

๐‘๐‘ธ ๐‘‡, ๐‘ก ๐‘‘๐‘‡

๐ถ๐‘„ ๐‘ก = ๐ถ๐‘† ๐‘‡โˆž

0

๐‘๐‘บ ๐‘‡, ๐‘ก ๐‘‘๐‘‡ = ๐ถ ๐‘† ๐‘ก

solute concentration at the catchment outlet

= ๐‘€๐‘† ๐‘ก /๐‘†(๐‘ก)

S(t)

more on the RS

7

Page 8: Paolo Benettin

many RS compartments one non-RS compartment

๐Ž (๐‘‡, ๐‘ก) ๐Ž (๐‘‡, ๐‘ก) ๐Ž (๐‘‡, ๐‘ก)

two practical approaches

need for a full hydrologic model (internal fluxes) incorporates catchment characteristics (easier)

based on data

8

Page 9: Paolo Benettin

DRAWBACKS โ€ข dry deposition โ€ข concentration is often too low (noise) โ€ข effect of plants: output conc. higher

than input conc.

9

chloride as a tracer

MAIN SOURCES โ€ข atmosphere (coastal areas) โ€ข agriculture (KCl is widely used) โ€ข (road salting)

TRACER? โ€ข mostly yes โ€ข no degradation โ€ข nutrient for plants, but in very low

concentrations

Page 10: Paolo Benettin

NL

outlet

10

chloride as a tracer

Hupsel Brook (NL)

Upper Hafren Plynlimon (UK)

fertilization fertilization

Page 11: Paolo Benettin

shorter (30-100 d) travel times

Q [

mm

/h]

longer (2-3 y) travel times

11

Hupsel Brook

Benettin et al., 2013, WRR

Page 12: Paolo Benettin

12

Upper Hafren, Plynlimon

longer travel times

shorter travel times

Benettin et al., 2015, WRR

Page 13: Paolo Benettin

water stable isotopes

13

MAIN SOURCES โ€ข atmosphere โ€ข (deutered water for small experiments)

liquid 2H, 18O

vapor

depleted enriched

2H, 18O

heavy

lighter lighter

Deuterium Hubbard Brook WS3 (USA)

Page 14: Paolo Benettin

14

water stable isotopes

TRACER? โ€ข mostly yes โ€ข from precipitation to discharge โ€ข if snowmelt and evaporation have

minor impact

precipitation

EPFL lysimeter (CH)

Hubbard Brook WS3 (USA)

Page 15: Paolo Benettin

MOBILE WATER

MINERAL

15

dissolved Si and Na

Hubbard Brook WS3 NH, USA

hydrologic transport in a forested catchment

Page 16: Paolo Benettin

NS= 0.62

16

deuterium transport

travel time distributions

Page 17: Paolo Benettin

Silicon (Si)

Nov-2006 Nov-2007 Nov-2008

dry days:

many old particles

wet days:

many young particles

๐ถ ๐‘ก = ๐ถ๐‘’๐‘ž 1 โˆ’ ๐‘’โˆ’๐‘˜๐‘ป ๐‘ ๐‘„ ๐‘ป, ๐‘ก ๐‘‘๐‘ป

โˆž

0

๐ถ๐‘’๐‘ž ๐‘(๐‘‡)

1ยฐ order chemical kinetics:

17

age-dependent transport

Page 18: Paolo Benettin

14-year dataset dissolved silicon and sodium

NS= 0.42 - 0.76

Silicon (Si) Sodium (Na)

NS= 0.34 - 0.66

1/๐‘˜ ~ 10 โˆ’ 13 ๐‘‘๐‘Ž๐‘ฆ๐‘ 

Benettin et al., in review 18

Page 19: Paolo Benettin

19

non-RS compartment

Queloz et al., 2015a,b, WRR

Injection of fluorobenzoate (FBA) tracers

Page 20: Paolo Benettin

20

ET

Q

fractional AGE older younger

validation

con

cen

trat

ion

[m

g/l

]

measurements

simulations

Q [

mm

/h]

mean age ~ 60-80 d โ€˜direct SAS approachโ€™

Page 21: Paolo Benettin

21

โ€ข simple hydrochemical models generate complex age dynamics

โ€ข use of age distributions to model geogenic solutes

โ€ข multi-RS system can efficiently reproduce emergent transport dynamics

โ€ข deeper exploration of โ€˜direct SASโ€™ approach

โ€ข characterization of the age of evapotranspiration

โ€ข move on to complex transport dynamics (e.g. nitrates)

Summary Future perspectives

Page 22: Paolo Benettin

acknowledgments

Plynlimon data:

Ype van der Velde

Hupsel Brook data:

Hubbard Brook data:

K.J. McGuire, S.W. Bailey, JP Gannon, M. Green, J. Campbell, G. Likens, D. Buso

ENAC/IIE/ECHO lab Pierre Queloz

Lysimeter data:

22


Top Related