Relationship between soil inorganic carbon and organic carbon in the wheat-maize cropland of the North China Plain

2017 ◽  
Vol 418 (1-2) ◽  
pp. 423-436 ◽  
Author(s):  
H. J. Shi ◽  
X. J. Wang ◽  
Y. J. Zhao ◽  
M. G. Xu ◽  
D. W. Li ◽  
...  
Keyword(s):  
Organic Carbon ◽  
North China Plain ◽  
North China ◽  
Inorganic Carbon ◽  
Soil Inorganic Carbon ◽  
The North ◽  
The North China Plain ◽  
Soil Inorganic

Carbonaceous components in particulate matter during a haze episode at a typical industrial area in the North China Plain

2020 ◽  
Vol ahead-of-print (ahead-of-print) ◽  
Author(s):  
Hongya Niu ◽  
Zhaoce Liu ◽  
Wei Hu ◽  
Wenjing Cheng ◽  
Mengren Li ◽  
...  
Keyword(s):  
Particulate Matter ◽  
Organic Carbon ◽  
North China Plain ◽  
North China ◽  
Large Fraction ◽  
Industrial Emissions ◽  
Content Type ◽  
The North ◽  
The North China Plain ◽  
The Mean

Purpose Severe airborne particulate pollution frequently occurs over the North China Plain (NCP) region in recent years. To better understand the characteristics of carbonaceous components in particulate matter (PM) over the NCP region. Design/methodology/approach PM samples were collected at a typical area affected by industrial emissions in Handan, in January 2016. The concentrations of organic carbon (OC) and elemental carbon (EC) in PM of different size ranges (i.e. PM2.5, PM10 and TSP) were measured. The concentrations of secondary organic carbon (SOC) were estimated by the EC tracer method. Findings The results show that the concentration of OC ranged from 14.9 μg m−3 to 108.4 μg m−3, and that of EC ranged from 4.0 μg m−3 to 19.4μg m−3, when PM2.5 changed from 58.0μg m−3 to 251.1μg m−3 during haze days, and the carbonaceous aerosols most distributed in PM2.5 rather than large fraction. The concentrations of OC and EC PM2.5 correlated better (r = 0.7) than in PM2.5−10 and PM>10, implying that primary emissions were dominant sources of OC and EC in PM2.5. The mean ratios of OC/EC in PM2.5, PM2.5–10 and PM>10 were 4.4 ± 2.1, 3.6 ± 0.9 and 1.9 ± 0.7, respectively. Based on estimation, SOC accounted for 16.3%, 22.0% and 9.1% in PM2.5, PM2.5–10 and PM>10 respectively. Originality/value The ratio of SOC/OC (48.2%) in PM2.5 was higher in Handan than those (28%–32%) in other megacities, e.g. Beijing, Tianjin and Shijiazhuang in the NCP, suggesting that the formation of SOC contributed significantly to OC. The mean mass absorption efficiencies of EC (MACEC) in PM10 and TSP were 3.4 m2 g−1 (1.9–6.6 m2 g−1) and 2.9 m2 g−1 (1.6–5.6 m2 g−1), respectively, both of which had similar variation patterns to those of OC/EC and SOC/OC.

scholarly journals Diurnal variations of organic molecular tracers and stable carbon isotopic composition in atmospheric aerosols over Mt. Tai in the North China Plain: an influence of biomass burning

2012 ◽  
Vol 12 (18) ◽  
pp. 8359-8375 ◽  
Author(s):  
P. Q. Fu ◽  
K. Kawamura ◽  
J. Chen ◽  
J. Li ◽  
Y. L. Sun ◽  
...  
Keyword(s):  
Organic Carbon ◽  
Biomass Burning ◽  
North China Plain ◽  
North China ◽  
Carbon Isotopic Composition ◽  
Organic Aerosol ◽  
Stable Carbon ◽  
Carbon Isotopic ◽  
The North ◽  
The North China Plain

Abstract. Organic tracer compounds, as well as organic carbon (OC), elemental carbon (EC), water-soluble organic carbon (WSOC), and stable carbon isotope ratios (δ13C) of total carbon (TC) have been investigated in aerosol samples collected during early and late periods of the Mount Tai eXperiment 2006 (MTX2006) field campaign in the North China Plain. Total solvent-extractable fractions were investigated by gas chromatography/mass spectrometry. More than 130 organic compounds were detected in the aerosol samples. They were grouped into twelve organic compound classes, including biomass burning tracers, biogenic primary sugars, biogenic secondary organic aerosol (SOA) tracers, and anthropogenic tracers such as phthalates, hopanes and polycyclic aromatic hydrocarbons (PAHs). In early June when the field burning activities of wheat straws in the North China Plain were very active, the total identified organics (2090 ± 1170 ng m−3) were double those in late June (926 ± 574 ng m−3). All the compound classes were more abundant in early June than in late June, except phthalate esters, which were higher in late June. Levoglucosan (88–1210 ng m−3, mean 403 ng m−3) was found as the most abundant single compound in early June, while diisobutyl phthalate was the predominant species in late June. During the biomass-burning period in early June, the diurnal trends of most of the primary and secondary organic aerosol tracers were characterized by the concentration peaks observed at mid-night or in early morning, while in late June most of the organic species peaked in late afternoon. This suggests that smoke plumes from biomass burning can uplift the aerosol particulate matter to a certain altitude, which could be further transported to and encountered the summit of Mt. Tai during nighttime. On the basis of the tracer-based method for the estimation of biomass-burning OC, fungal-spore OC and biogenic secondary organic carbon (SOC), we estimate that an average of 24% (up to 64%) of the OC in the Mt. Tai aerosols was due to biomass burning in early June, followed by the contribution of isoprene SOC (mean 4.3%). In contrast, isoprene SOC was the main contributor (6.6%) to OC, and only 3.0% of the OC was due to biomass burning in late June. In early June, δ13C of TC (−26.6 to −23.2‰, mean −25.0‰) were lower than those (−23.9 to −21.9‰, mean −22.9‰) in late June. In addition, a strong anti-correlation was found between levoglucosan and δ13C values. This study demonstrates that crop-residue burning activities can significantly enhance the organic aerosol loading and alter the organic composition and stable carbon isotopic composition of aerosol particles in the troposphere over the North China Plain.

Effects of soil moisture and nitrogen addition on organic carbon mineralization in a high-yield cropland soil of the North China Plain

2014 ◽  
Vol 34 (14) ◽  
Author(s):  
李银坤 LI Yinkun ◽  
陈敏鹏 CHEN Minpeng ◽  
梅旭荣 MEI Xurong ◽  
夏 旭 XIA Xu ◽  
郭文忠 GUO Wenzhong ◽  
...  
Keyword(s):  
Soil Moisture ◽  
Organic Carbon ◽  
North China Plain ◽  
North China ◽  
Carbon Mineralization ◽  
Nitrogen Addition ◽  
High Yield ◽  
The North ◽  
The North China Plain ◽  
Organic Carbon Mineralization
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