Environmental controls on the stable carbon isotopic composition of soil organic carbon: implications for modelling the distribution of C3and C4plants, Australia

Tellus B ◽  
2008 ◽  
Vol 60 (4) ◽  
Author(s):  
Jonathan G. Wynn ◽  
Michael I. Bird
Keyword(s):  
Organic Carbon ◽  
Soil Organic Carbon ◽  
Isotopic Composition ◽  
Carbon Isotopic Composition ◽  
Stable Carbon ◽  
Carbon Isotopic ◽  
Environmental Controls

The Distribution and Stable Carbon Isotopic Composition of Dissolved Organic Carbon in Estuaries

Estuaries ◽  
1994 ◽  
Vol 17 (1) ◽  
pp. 111 ◽  
Author(s):  
Bruce Peterson ◽  
Brian Fry ◽  
Meredith Hullar ◽  
Susan Saupe ◽  
Richard Wright
Keyword(s):  
Organic Carbon ◽  
Dissolved Organic Carbon ◽  
Isotopic Composition ◽  
Carbon Isotopic Composition ◽  
Stable Carbon ◽  
Carbon Isotopic

scholarly journals Springtime carbon episodes at Gosan background site revealed by total carbon, stable carbon isotopic composition, and thermal characteristics of carbonaceous particles

2011 ◽  
Vol 11 (5) ◽  
pp. 13867-13910
Author(s):  
J. Jung ◽  
K. Kawamura
Keyword(s):  
Citric Acid ◽  
Organic Carbon ◽  
Isotopic Composition ◽  
Thermal Evolution ◽  
Carbon Isotopic Composition ◽  
Organic Aerosols ◽  
Total Carbon ◽  
Stable Carbon ◽  
Carbon Isotopic ◽  
Airborne Pollens

Abstract. In order to investigate the carbon episodes at Gosan background super-site (33.17° N, 126.10° E) in East Asia during spring of 2007 and 2008, total suspended particles (TSP) were collected and analyzed for particulate organic carbon, elemental carbon, total carbon (TC), total nitrogen (TN), and stable carbon isotopic composition (δ13C) of TC. The carbon episodes at the Gosan site were categorized as long-range transported anthropogenic pollutant (LTP) from Asian continent, Asian dust (AD) accompanying with LTP, and local pollen episodes. The stable carbon isotopic composition of TC (δ13CTC) was found to be lowest during the pollen episodes (range: −26.2 ‰ to −23.5 ‰, avg.: −25.2 ± 0.9 ‰), followed by the LTP episodes (range: −23.5 ‰ to −23.0 ‰, avg.: −23.3 ± 0.3 ‰) and the AD episodes (range: −23.3 to −20.4 %, avg.: −21.8 ± 2.0 ‰). The δ13CTC of the airborne pollens (−28.0 ‰) collected at the Gosan site showed value similar to that of tangerine fruit (−28.1 ‰) produced from Jeju Island. Based on the carbon isotope mass balance equation and the TN and TC regression approach, we found that ∼40–45 % of TC in the TSP samples during the pollen episodes was attributed to airborne pollens from Japanese cedar trees planted around tangerine farms in Jeju Island. The δ13C of citric acid in the airborne pollens (−26.3 ‰) collected at the Gosan site was similar to that in tangerine fruit (−27.4 ‰). The negative correlation between the citric acid-carbon/TC ratios and δ13CTC were obtained during the pollen episodes. These results suggest that citric acid emitted from tangerine fruit may be adsorbed on the airborne pollens and then transported to the Gosan site. Based on the thermal evolution pattern of organic aerosols during the carbon episodes, we found that organic aerosols originated from East China are more volatile on heating and are more likely to form pyrolized organic carbon than the pollen-enriched organic aerosols and organic aerosols originated from Northeast China. Since thermal evolution patterns of organic aerosols are highly influenced by their molecular weight, they can be used as additional information on the formation of secondary organic aerosols during the long-range atmospheric transport and the source regions of organics.

scholarly journals Springtime carbon emission episodes at the Gosan background site revealed by total carbon, stable carbon isotopic composition, and thermal characteristics of carbonaceous particles

2011 ◽  
Vol 11 (21) ◽  
pp. 10911-10928 ◽  
Author(s):  
J. Jung ◽  
K. Kawamura
Keyword(s):  
Citric Acid ◽  
Organic Carbon ◽  
Isotopic Composition ◽  
Thermal Evolution ◽  
Airborne Pollen ◽  
Carbon Isotopic Composition ◽  
Organic Aerosols ◽  
Total Carbon ◽  
Stable Carbon ◽  
Carbon Isotopic

Abstract. In order to investigate the emission of carbonaceous aerosols at the Gosan background super-site (33.17° N, 126.10° E) in East Asia, total suspended particles (TSP) were collected during spring of 2007 and 2008 and analyzed for particulate organic carbon, elemental carbon, total carbon (TC), total nitrogen (TN), and stable carbon isotopic composition (δ13C) of TC. The stable carbon isotopic composition of TC (δ13CTC) was found to be lowest during pollen emission episodes (range: −26.2‰ to −23.5‰, avg. −25.2 ± 0.9‰), approaching those of the airborne pollen (−28.0‰) collected at the Gosan site. Based on a carbon isotope mass balance equation, we found that ~42% of TC in the TSP samples during the pollen episodes was attributed to airborne pollen from Japanese cedar trees planted around tangerine farms in Jeju Island. A negative correlation between the citric acid-carbon/TC ratios and δ13CTC was obtained during the pollen episodes. These results suggest that citric acid emitted from tangerine fruit may be adsorbed on the airborne pollen and then transported to the Gosan site. Thermal evolution patterns of organic carbon during the pollen episodes were characterized by high OC evolution in the OC2 temperature step (450 °C). Since thermal evolution patterns of organic aerosols are highly influenced by their molecular weight, they can be used as additional information on the formation of secondary organic aerosols and the effect of aging of organic aerosols during the long-range atmospheric transport and sources of organic aerosols.

scholarly journals Stable carbon isotopic composition of light hydrocarbons and n-alkanes of condensates in the Tarim Basin, NW China

2017 ◽  
Vol 2 (3) ◽  
pp. 165-177 ◽  
Author(s):  
Shipeng Huang ◽  
Chenchen Fang ◽  
Weilong Peng ◽  
Qingchun Jiang ◽  
Ziqi Feng
Keyword(s):  
Isotopic Composition ◽  
Tarim Basin ◽  
Carbon Isotopic Composition ◽  
Stable Carbon ◽  
Light Hydrocarbons ◽  
Nw China ◽  
Carbon Isotopic
Sign in / Sign up

Export Citation Format

Share Document