AustralieFrV1, PascalFrancis, Corpus, bibRecord, 000634

Major 20th century changes of water-soluble humic-like substances (HULISWS) aerosol over Europe inferred from Alpine ice cores

Identifieur interne : 000634 ( PascalFrancis/Corpus ); précédent : 000633; suivant : 000635

Major 20th century changes of water-soluble humic-like substances (HULISWS) aerosol over Europe inferred from Alpine ice cores

Auteurs : J. Guilhermet ; S. Preunkert ; D. Voisin ; C. Baduel ; M. Legrand

Source :

Journal of geophysical research. Atmospheres : (Print) [ 2169-897X ] ; 2013.

RBID : Pascal:14-0009278

Descripteurs français

Pascal (Inist)
- Siècle 20eme, Aérosol, Carotte, Carbone organique total, Matière organique, Variation saisonnière, Analyse tendance, Facteur biogène, Précurseur, Glace, Europe, Alpes Françaises.

English descriptors

KwdEn :
- Biogenic factor, Century 20th, Europe, French Alps, Precursor, Total organic carbon, aerosols, drill cores, ice, organic materials, seasonal variations, trend-surface analysis.

Abstract

Using a newly developed method dedicated to measurements of water-soluble humic-like substances (HULIS_WS) in atmospheric aerosol samples, the carbon mass quantification of HULIS_WS in an Alpine ice core is achieved for the first time. The method is based on the extraction of HULIS_WS with a weak anion-exchanger resin and the subsequent quantification of the extracted carbon fraction with a total organic carbon (TOC) analyzer. Measurements were performed along a Col du Dôme (4250 m above sea level, French Alps) ice core covering the 1920-2004 time period. The HULIS_WS concentrations exhibit a well-marked seasonal cycle with winter minima close to 7 ppbC and summer maxima ranging between 10 and 50 ppbC. Whereas the winter HULIS_WS concentrations remained unchanged over the twentieth century, the summer concentrations increased from 20 ppbC prior to the Second World War to 35 ppbC in the 1970-1990s. These different trends reflect the different types of HULIS_WS sources in winter and summer. HULIS_WS are mainly primarily emitted by domestic wood burning in winter and secondary in summer being produced from biogenic precursors. For unknown reason, the HULIS_WS signal is found to be unusual in ice samples corresponding to World War II.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A03		`1`		`@0 J. geophys. res., Atmos. : (Print)`
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A11	`02`	`1`		`@1 PREUNKERT (S.)`
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A11	`04`	`1`		`@1 BADUEL (C.)`
A11	`05`	`1`		`@1 LEGRAND (M.)`
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A43	`01`			`@1 INIST @2 3144D1 @5 354000140724180320`
A44				`@0 0000 @1 © 2014 INIST-CNRS. All rights reserved.`
A45				`@0 1 p.1/2`
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A64	`01`	`1`		`@0 Journal of geophysical research. Atmospheres : (Print)`
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C01	`01`		`ENG`	@0 Using a newly developed method dedicated to measurements of water-soluble humic-like substances (HULIS_WS) in atmospheric aerosol samples, the carbon mass quantification of HULIS_WS in an Alpine ice core is achieved for the first time. The method is based on the extraction of HULIS_WS with a weak anion-exchanger resin and the subsequent quantification of the extracted carbon fraction with a total organic carbon (TOC) analyzer. Measurements were performed along a Col du Dôme (4250 m above sea level, French Alps) ice core covering the 1920-2004 time period. The HULIS_WS concentrations exhibit a well-marked seasonal cycle with winter minima close to 7 ppbC and summer maxima ranging between 10 and 50 ppbC. Whereas the winter HULIS_WS concentrations remained unchanged over the twentieth century, the summer concentrations increased from 20 ppbC prior to the Second World War to 35 ppbC in the 1970-1990s. These different trends reflect the different types of HULIS_WS sources in winter and summer. HULIS_WS are mainly primarily emitted by domestic wood burning in winter and secondary in summer being produced from biogenic precursors. For unknown reason, the HULIS_WS signal is found to be unusual in ice samples corresponding to World War II.
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C03	`06`	`2`	`SPA`	`@0 Variación estacional @5 06`
C03	`07`	`2`	`FRE`	`@0 Analyse tendance @5 09`
C03	`07`	`2`	`ENG`	`@0 trend-surface analysis @5 09`
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C03	`08`	`X`	`FRE`	`@0 Facteur biogène @5 10`
C03	`08`	`X`	`ENG`	`@0 Biogenic factor @5 10`
C03	`08`	`X`	`SPA`	`@0 Factor biógeno @5 10`
C03	`09`	`X`	`FRE`	`@0 Précurseur @5 11`
C03	`09`	`X`	`ENG`	`@0 Precursor @5 11`
C03	`09`	`X`	`SPA`	`@0 Precursor @5 11`
C03	`10`	`2`	`FRE`	`@0 Glace @5 12`
C03	`10`	`2`	`ENG`	`@0 ice @5 12`
C03	`10`	`2`	`SPA`	`@0 Hielo @5 12`
C03	`11`	`2`	`FRE`	`@0 Europe @2 564 @5 21`
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Format Inist (serveur)

NO :	PASCAL 14-0009278 INIST
ET :	Major 20th century changes of water-soluble humic-like substances (HULIS_WS) aerosol over Europe inferred from Alpine ice cores
AU :	GUILHERMET (J.); PREUNKERT (S.); VOISIN (D.); BADUEL (C.); LEGRAND (M.)
AF :	UJF-Grenoble 1/CNRS, Laboratoire de Glaciologie et Géophysique de l'Environnement (LGGE) UMR 5183/Grenoble 38041/France (1 aut., 2 aut., 3 aut., 4 aut., 5 aut.); National Research Centre for Environmental Toxicology (Entox)/Coopers Plains, Queensland 4108/Australie (4 aut.)
DT :	Publication en série; Niveau analytique
SO :	Journal of geophysical research. Atmospheres : (Print); ISSN 2169-897X; Etats-Unis; Da. 2013; Vol. 118; No. 9; Pp. 3869-3878; Bibl. 1 p.1/2
LA :	Anglais
EA :	Using a newly developed method dedicated to measurements of water-soluble humic-like substances (HULIS_WS) in atmospheric aerosol samples, the carbon mass quantification of HULIS_WS in an Alpine ice core is achieved for the first time. The method is based on the extraction of HULIS_WS with a weak anion-exchanger resin and the subsequent quantification of the extracted carbon fraction with a total organic carbon (TOC) analyzer. Measurements were performed along a Col du Dôme (4250 m above sea level, French Alps) ice core covering the 1920-2004 time period. The HULIS_WS concentrations exhibit a well-marked seasonal cycle with winter minima close to 7 ppbC and summer maxima ranging between 10 and 50 ppbC. Whereas the winter HULIS_WS concentrations remained unchanged over the twentieth century, the summer concentrations increased from 20 ppbC prior to the Second World War to 35 ppbC in the 1970-1990s. These different trends reflect the different types of HULIS_WS sources in winter and summer. HULIS_WS are mainly primarily emitted by domestic wood burning in winter and secondary in summer being produced from biogenic precursors. For unknown reason, the HULIS_WS signal is found to be unusual in ice samples corresponding to World War II.
CC :	001E02D
FD :	Siècle 20eme; Aérosol; Carotte; Carbone organique total; Matière organique; Variation saisonnière; Analyse tendance; Facteur biogène; Précurseur; Glace; Europe; Alpes Françaises
FG :	Alpes
ED :	Century 20th; aerosols; drill cores; Total organic carbon; organic materials; seasonal variations; trend-surface analysis; Biogenic factor; Precursor; ice; Europe; French Alps
EG :	Alps
SD :	Siglo 20; Aerosol; Testigo; Carbono orgánico total; Materia orgánica; Variación estacional; Análisis tendencia; Factor biógeno; Precursor; Hielo; Europa; Alpes Franceses
LO :	INIST-3144D1.354000140724180320
ID :	14-0009278

Links to Exploration step

Pascal:14-0009278

Le document en format XML

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<front><div type="abstract" xml:lang="en">Using a newly developed method dedicated to measurements of water-soluble humic-like substances (HULIS<sub>WS</sub>
) in atmospheric aerosol samples, the carbon mass quantification of HULIS<sub>WS</sub>
 in an Alpine ice core is achieved for the first time. The method is based on the extraction of HULIS<sub>WS</sub>
 with a weak anion-exchanger resin and the subsequent quantification of the extracted carbon fraction with a total organic carbon (TOC) analyzer. Measurements were performed along a Col du Dôme (4250 m above sea level, French Alps) ice core covering the 1920-2004 time period. The HULIS<sub>WS</sub>
 concentrations exhibit a well-marked seasonal cycle with winter minima close to 7 ppbC and summer maxima ranging between 10 and 50 ppbC. Whereas the winter HULIS<sub>WS</sub>
 concentrations remained unchanged over the twentieth century, the summer concentrations increased from 20 ppbC prior to the Second World War to 35 ppbC in the 1970-1990s. These different trends reflect the different types of HULIS<sub>WS</sub>
 sources in winter and summer. HULIS<sub>WS</sub>
 are mainly primarily emitted by domestic wood burning in winter and secondary in summer being produced from biogenic precursors. For unknown reason, the HULIS<sub>WS</sub>
 signal is found to be unusual in ice samples corresponding to World War II.</div>
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<fC01 i1="01" l="ENG"><s0>Using a newly developed method dedicated to measurements of water-soluble humic-like substances (HULIS<sub>WS</sub>
) in atmospheric aerosol samples, the carbon mass quantification of HULIS<sub>WS</sub>
 in an Alpine ice core is achieved for the first time. The method is based on the extraction of HULIS<sub>WS</sub>
 with a weak anion-exchanger resin and the subsequent quantification of the extracted carbon fraction with a total organic carbon (TOC) analyzer. Measurements were performed along a Col du Dôme (4250 m above sea level, French Alps) ice core covering the 1920-2004 time period. The HULIS<sub>WS</sub>
 concentrations exhibit a well-marked seasonal cycle with winter minima close to 7 ppbC and summer maxima ranging between 10 and 50 ppbC. Whereas the winter HULIS<sub>WS</sub>
 concentrations remained unchanged over the twentieth century, the summer concentrations increased from 20 ppbC prior to the Second World War to 35 ppbC in the 1970-1990s. These different trends reflect the different types of HULIS<sub>WS</sub>
 sources in winter and summer. HULIS<sub>WS</sub>
 are mainly primarily emitted by domestic wood burning in winter and secondary in summer being produced from biogenic precursors. For unknown reason, the HULIS<sub>WS</sub>
 signal is found to be unusual in ice samples corresponding to World War II.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>001E02D</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE"><s0>Siècle 20eme</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG"><s0>Century 20th</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA"><s0>Siglo 20</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Aérosol</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>aerosols</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>Aerosol</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Carotte</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>drill cores</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="SPA"><s0>Testigo</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Carbone organique total</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Total organic carbon</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Carbono orgánico total</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Matière organique</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>organic materials</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Materia orgánica</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Variation saisonnière</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>seasonal variations</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Variación estacional</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Analyse tendance</s0>
<s5>09</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>trend-surface analysis</s0>
<s5>09</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Análisis tendencia</s0>
<s5>09</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Facteur biogène</s0>
<s5>10</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Biogenic factor</s0>
<s5>10</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Factor biógeno</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Précurseur</s0>
<s5>11</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Precursor</s0>
<s5>11</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Precursor</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Glace</s0>
<s5>12</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>ice</s0>
<s5>12</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Hielo</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Europe</s0>
<s2>564</s2>
<s5>21</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>Europe</s0>
<s2>564</s2>
<s5>21</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Europa</s0>
<s2>564</s2>
<s5>21</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Alpes Françaises</s0>
<s2>NG</s2>
<s5>22</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>French Alps</s0>
<s2>NG</s2>
<s5>22</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Alpes Franceses</s0>
<s2>NG</s2>
<s5>22</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Alpes</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Alps</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Alpes</s0>
<s2>NG</s2>
</fC07>
<fN21><s1>006</s1>
</fN21>
</pA>
</standard>
<server><NO>PASCAL 14-0009278 INIST</NO>
<ET>Major 20th century changes of water-soluble humic-like substances (HULIS<sub>WS</sub>
) aerosol over Europe inferred from Alpine ice cores</ET>
<AU>GUILHERMET (J.); PREUNKERT (S.); VOISIN (D.); BADUEL (C.); LEGRAND (M.)</AU>
<AF>UJF-Grenoble 1/CNRS, Laboratoire de Glaciologie et Géophysique de l'Environnement (LGGE) UMR 5183/Grenoble 38041/France (1 aut., 2 aut., 3 aut., 4 aut., 5 aut.); National Research Centre for Environmental Toxicology (Entox)/Coopers Plains, Queensland 4108/Australie (4 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Journal of geophysical research. Atmospheres : (Print); ISSN 2169-897X; Etats-Unis; Da. 2013; Vol. 118; No. 9; Pp. 3869-3878; Bibl. 1 p.1/2</SO>
<LA>Anglais</LA>
<EA>Using a newly developed method dedicated to measurements of water-soluble humic-like substances (HULIS<sub>WS</sub>
) in atmospheric aerosol samples, the carbon mass quantification of HULIS<sub>WS</sub>
 in an Alpine ice core is achieved for the first time. The method is based on the extraction of HULIS<sub>WS</sub>
 with a weak anion-exchanger resin and the subsequent quantification of the extracted carbon fraction with a total organic carbon (TOC) analyzer. Measurements were performed along a Col du Dôme (4250 m above sea level, French Alps) ice core covering the 1920-2004 time period. The HULIS<sub>WS</sub>
 concentrations exhibit a well-marked seasonal cycle with winter minima close to 7 ppbC and summer maxima ranging between 10 and 50 ppbC. Whereas the winter HULIS<sub>WS</sub>
 concentrations remained unchanged over the twentieth century, the summer concentrations increased from 20 ppbC prior to the Second World War to 35 ppbC in the 1970-1990s. These different trends reflect the different types of HULIS<sub>WS</sub>
 sources in winter and summer. HULIS<sub>WS</sub>
 are mainly primarily emitted by domestic wood burning in winter and secondary in summer being produced from biogenic precursors. For unknown reason, the HULIS<sub>WS</sub>
 signal is found to be unusual in ice samples corresponding to World War II.</EA>
<CC>001E02D</CC>
<FD>Siècle 20eme; Aérosol; Carotte; Carbone organique total; Matière organique; Variation saisonnière; Analyse tendance; Facteur biogène; Précurseur; Glace; Europe; Alpes Françaises</FD>
<FG>Alpes</FG>
<ED>Century 20th; aerosols; drill cores; Total organic carbon; organic materials; seasonal variations; trend-surface analysis; Biogenic factor; Precursor; ice; Europe; French Alps</ED>
<EG>Alps</EG>
<SD>Siglo 20; Aerosol; Testigo; Carbono orgánico total; Materia orgánica; Variación estacional; Análisis tendencia; Factor biógeno; Precursor; Hielo; Europa; Alpes Franceses</SD>
<LO>INIST-3144D1.354000140724180320</LO>
<ID>14-0009278</ID>
</server>
</inist>
</record>

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Major 20th century changes of water-soluble humic-like substances (HULISWS) aerosol over Europe inferred from Alpine ice cores

Major 20th century changes of water-soluble humic-like substances (HULISWS) aerosol over Europe inferred from Alpine ice cores

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