Cont ontribut ibution ion of of Rus ussian ian ter erres - - PowerPoint PPT Presentation

cont ontribut ibution ion of of rus ussian ian
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Cont ontribut ibution ion of of Rus ussian ian ter erres - - PowerPoint PPT Presentation

Cont ontribut ibution ion of of Rus ussian ian ter erres estrial ial ecos ecosystems ems to o global lobal soil oil res espir piration ion flux lux Irina N. Kurganova Institute of Physicochemical and Biological Problems in Soil


slide-1
SLIDE 1

Cont

  • ntribut

ibution ion of

  • f Rus

ussian ian ter erres estrial ial ecos ecosystems ems to

  • global

lobal soil

  • il res

espir piration ion flux lux

Institute of Physicochemical and Biological Problems in Soil Science, RAS, Pushchino, Moscow region, Russia

Irina N. Kurganova

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

slide-2
SLIDE 2

The global CO2 flux from soils is an important regulator of climate change as well as determinant of net ecosystem C balance (Baggs, 2006). The territory of Russia occupies more than 1/9 of the land surface. The role of Russian soils in the global carbon cycle is very considerable; Therefore, more accurate estimates of the carbon fluxes from the terrestrial ecosystems of Russia should be obtained.

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

INT NTROD ODUC UCTION ON

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SLIDE 3

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

  • Tot
  • tal

al res espir piration ion flux: lux: 3.12 3.12 Pg g C yr yr-1

  • 1 -
  • only for growing period

(Kudeyarov et al., 1995); 4.50 4.50 Pg g C yr yr-1

  • 1 -
  • for whole year (Kudeyarov,

Kurganova, 1998);

  • Micr

icrobial

  • bial res

espir piration ion flux: lux: 2.60-3.05 2.60-3.05 Pg g C yr-1

  • 1(Kudeyarov, 2000; Nilsson et

al., 2000).

Previous ious es estima imates es of

  • f tot
  • tal

al and and micr microbial

  • bial

res espir piration ion for

  • r Rus

ussian ian ter errit itor

  • ry:
slide-4
SLIDE 4

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

(1) gather and analyze the database on soil respiration in Russia; (2) develop a model for the assessment of the annual CO2 fluxes from soils on the basis of summer CO2 fluxes

  • bservations;

(3) calculate the total respiration flux from Russian soils for the whole territory of Russia with the use of geo- information technologies.

This his study udy was as aimed aimed to:

  • :
slide-5
SLIDE 5

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

Anal nalysis is of

  • f soil
  • il res

espir piration ion da databas base

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SLIDE 6

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

Loca Location ion of

  • f sit

ites es on

  • n soil
  • il res

espir piration ion (SR) meas measur urement ements

slide-7
SLIDE 7

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

50 100 150 200 250 300 350

January February March A pril May June July A ugust September October November December

His Histog

  • gram

am of

  • f SR meas

measur urement ements accor according ding to

  • dif

differ erent ent mont months hs

slide-8
SLIDE 8

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

10 20 30 40 50

Summer C-СО2 flux, gСm-2

0-50 51-100 101-150 151-200 201-250 251-300 301-350 351-400 401-450 451-500 501-550 551-600 601-650 651-700 701-750

His Histog

  • gram

am of

  • f summer

ummer CO2 flux luxes es from

  • m soils
  • ils in

in Rus ussian ian ter erres estrial ial ecos ecosystems ems

Mean value -222 g C m-2 Median value - 190g C m-2

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SLIDE 9

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

Development elopment of

  • f model

model for

  • r

the he as asses essment ment of

  • f the

he annual annual CO2 flux luxes es

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SLIDE 10

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

Mean annual, CS, % Reference N Soil Vegetation air T,oC 1 Podbur tundra Moss-lichen

  • 13,4

90,2 Zamolodchikov, Karelin, 2001 2 Podbur tundra Moss-lichen

  • 11,8

91,3 Zamolodchikov, Karelin, 2001 3 Podbur tundra Moss-lichen

  • 7,4

84,2 Zamolodchikov, Karelin, 2001 4 Podbur tundra Moss-lichen

  • 6,4

91,0 Zamolodchikov, Karelin, 2001 5 Sandy soil Spruse forest 2 45,0 Havas&Maenpaa, 1972 6 Sod-podzolic Forest mixed 4,0 45,6 Lopes de Gerenyu et al., 2001 7 Sod podzolic Grassland 4,0 45,6 Lopes de Gerenyu et al., 2001 8 Grey forest soil Forest Mixed 4,0 48,8 Lopes de Gerenyu et al., 2001 9 Grey forest soil Grassland 4,0 43,1 Lopes de Gerenyu et al., 2001 10 Grey forest soil Arable 4,0 51,6 Lopes de Gerenyu et al., 2001 11 Podzol (iron) Pine (scots) forest 4,4 47,3 Pajary, 1995 12 Podzol (iron) Pine (scots) forest 4,4 51,4 Pajary, 1995 13 Loamy sandy Beech-spruce forest 6,5 35,9 Dorr&Munich.,1987 14 Peat-bog Low bog 6,5 44,0 Adam, Star, 1997 15 Brownerde Spruce Forest 6,5 46,9 Adam, Star, 1997 16 Kolluvisol Grassland 6,5 34,8 Adam, Star, 1997 17 Soil Crops 8,4 32,9 Monteith et al., 1964 18 Soil Sweet Chestnut 10,5 37,4 Anderson, 1973 19 Soil Beech 10,5 40,9 Anderson, 1973

Mean ean annual annual air air temper emperatur ure e and and shar hare e of

  • f

summer ummer CO2 flux lux (CS) to

  • the

he annual annual CO2 flux lux

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SLIDE 11

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

Models

  • dels for
  • r calcula

calculation ion of

  • f tot
  • tal

al annual annual CO CO2 flux lux (AF) F): :

Cs Cs - contribution

  • f summer CO2

flux (Fs) to AF, %; Ta Ta- mean annual air temperature,

  • C;

Cs = 0,014Ta

3 + 0,035Ta 2

  • 4,07Ta + 61,5

R

2 = 0,95

СS = -2,71Ta + 59,7 R

2 = 0,91 20 40 60 80 100 120

  • 15
  • 10
  • 5

5 10 15

Mean annual air temperature,

  • C

Contribution of summer CO2 flux to AF, Cs %

We e kno know (from

  • m da

data a bas base) e):

  • summer CO2 flux Fs;
  • mean annual air

temperature, Ta; a;

We can calculate:

Cs (according to model),

AF F = Fs Fs * 100 100 / Cs

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SLIDE 12

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

10 20 30 40 50 60

1-100 101-200 201-300 301-400 401-500 501-600 601-700 701-800 801-900 901-1000 1001-1100 1101-1200 1201-1300 1301-1400 1401-1500 1501-1600 1601-1700

СО2 flux, g С m

  • 2

Number of ecosystems

Average flux - 469 g C m-2 Median value - 395 g C m-2

His Histog

  • gram

am of

  • f annual

annual CO2 flux luxes es from

  • m soils
  • ils in

in Rus ussian ian for

  • res

est zone

  • ne
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SLIDE 13

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

Estima imate e of

  • f tot
  • tal

al res espir piration ion flux lux from

  • m

Rus ussian ian soils

  • ils
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SLIDE 14

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

Soil

  • il div

divis ision ion and and soil

  • il res

espir piration ion ma maps ps

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SLIDE 15

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

Parameter World Russia

abs.units %

Area, million km2 148.65 17.08 11.5 NPP , Gt С/yr 60 4.41 7.4 TSR, Gt С/yr 64-72 5.67 7.9-9.3 Industrial СО2 emission, Gt С/yr 7.7 0.41 2.5 Soil organic C pool (0-100cm), Gt C 1500 296 20 C-balance, Gt С/yr

2.7 2.7 0.91 0.91

33.7

Cont

  • ntribut

ibution ion of

  • f Rus

ussian ian ter erres estrial ial ecos ecosystems ems to

  • global

lobal C-f

  • flux

luxes es

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SLIDE 16

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

Conc

  • nclus

lusions ions:

Ш The presented estimation of total CO2 flux from Russian terrestrial ecosystems (5.67 Gt/yr) could be approximately addressed to the 1990s – the initial period of Kyoto Protocol. Ш Uncertainties of this estimation depend upon amount and quality of available experimental data, accuracy and resolution of the soil map at scale 1:5 million, spatial aggregation techniques and regression models used. Ш To update this estimate, it needs to increase the numbers and the geographical representatives of long- term measurements, and to use up-to-date areas of croplands, grasslands and forests on Russian territory.

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SLIDE 17

ENVIROMIS-2010, 5-11 July 2010, Tomsk, Russia

Thank hank you

  • u for
  • r attent

ention! ion!