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Journal ArticleDOI

The importance of non-fossil sources in carbonaceous aerosols in a megacity of central China during the 2013 winter haze episode: A source apportionment constrained by radiocarbon and organic tracers

TL;DR: In this paper, a source apportionment of different carbonaceous aerosols (CAs) was conducted in a megacity in central China (Wuhan, Hubei Province) by using the measurements of radiocarbon and molecular organic tracers.
About: This article is published in Atmospheric Environment.The article was published on 2016-11-01 and is currently open access. It has received 26 citations till now. The article focuses on the topics: Haze & Total organic carbon.

Summary (3 min read)

Introduction

  • Testing for anaemia in pregnancy is ubiquitous across low and high income countries and usually begins at the booking (first antenatal) appointment.
  • Screening may range from looking for risk factors and clinical features of anaemia in the history, to point of care testing or laboratory assessment of the full blood count with or without assessment of iron parameters from a venous sample.
  • (1) Which of these provides the most reliable and cost effective assessment remains unanswered.
  • The authors will provide an overview of the landscape of the literature surrounding the use of haemoglobin as a screening tool for anaemia in pregnancy, the implications this has on clinical care, resource allocation and national and international policy.

Why is anaemia screening important?

  • It is widely acknowledged that anaemia in pregnancy is associated with significant morbidity and mortality (if severe) for the mother, independently of other factors.
  • (3) Anaemia has also been associated with adverse outcomes for the developing baby, including low birth weight and preterm delivery.
  • This reduces the need for additional screening tests and avoids delays in management.
  • (8) This may make a case for routine iron supplementation.
  • (7) The ongoing high prevalence of anaemia globally and the lack of evidence demonstrating safety and efficacy of routine iron supplementation in pregnancy highlights unmet clinical and research needs.

Low and middle income countries

  • More than 1.6 billion people are anaemic, with 42% of all pregnant women worldwide affected.
  • In these settings the causes of anaemia are often complex, however the global focus currently remains on iron deficiency anaemia.
  • (1) Those found to be anaemic should be offered daily iron supplementation and those not yet anaemic offered iron and folic acid weekly.
  • Below the authors discuss a few key issues briefly.
  • (16) While each micronutrients have specific roles, multiple deficiencies tend to cluster within individuals, acting synergistically increasing the burden of disease.

Soil-transmitted helminths

  • Infectious diseases such as hookworm reduce absorption and metabolism of key micronutrients (notably iron) in addition to increasing gastrointestinal tract losses.
  • Hookworm infections contribute greatly to the high prevalence of anaemia in sub-Saharan Africa and Southeast Asia, with an estimated 576–740 million infections.
  • There are clear benefits from pooled estimates of randomized controlled trials of deworming and concomitant iron supplementation strategies showing improvements in mean haemoglobin concentration across sub-Saharan Africa. (18).
  • As a result, the current WHO recommendation for preventive chemotherapy include using single-dose albendazole (400 mg) or mebendazole (500 mg), as a public health intervention for pregnant women, after the first trimester, living in areas where both anaemia and soil transmitted helminth infections are considered endemic. (19).

Malaria

  • Malarial infection, particularly plasmodium falciparum can lead to and worsen preexisting anaemia.
  • (20) The balance of iron supplementation in the context of malarial infection (suspected or confirmed) requires careful consideration; it has been an area of considerable debate.
  • (20, 21) In areas such as Africa, WHO recommends prevention and treatment of malaria during pregnancy using of long-lasting insecticidal nets ; in all areas with moderate to high malaria transmission in Africa, intermittent preventive treatment in pregnancy (IPTP) with sulfadoxine-pyrimethamine (SP), as part of antenatal care services and prompt diagnosis and effective treatment of malaria infections.

Genetic causes

  • Haemoglobin disorders affect populations in LMICs disproportionately more than other areas of the world, particularly Africa and South East Asian regions where 18.2% and 6.6% of the population, respectively, carry a significant haemoglobin variant, as a result affecting more than 7% of pregnant women worldwide.
  • Values of haemoglobin below this disease defining threshold necessitate treatment, but cannot suggest what treatment should be offered, as a fall in haemoglobin is multifactorial.
  • There is increasing awareness that the evidence base behind widely used thresholds for anaemia and iron biomarkers in pregnancy is poor.
  • Currently there is ongoing work by WHO to look at the evidence behind anaemia defining haemoglobin levels used in clinical practice and research, which may change the tide in this area.
  • As a consequence, guidelines and policy may be frustratingly vague.

What next?

  • There are emerging Australian data suggesting testing and treatment of non-anaemic iron deficiency would be beneficial in reducing transfusion post-delivery, however this has not been tested in trial settings.
  • (38) There are limited data on the use of other laboratory tests as screening tools.
  • In routine clinical practice a low haemoglobin, mean cell volume (MCV) and mean cell haemoglobin (MCH), and mean cell haemoglobin concentration (MCHC) are suggestive of iron deficiency, but need cautious interpretation.
  • Further testing and cost effectiveness analyses would be required before this could be implemented outside of research.
  • (28) Other markers such as serum hepcidin (a key homeostatic regulator of iron metabolism) are currently being tested in pregnancy settings, but are not routinely available for clinical use. (41).

Conclusion

  • Haemoglobin is still widely used as a screening tool for anaemia in pregnancy.
  • In the UK, a fall in haemoglobin is most commonly as a result of iron deficiency and so current guidelines recommend oral iron therapy as first line management.
  • In LMIC settings, iron supplementation alone is unlikely to improve anaemia prevalence.

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Citations
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Journal ArticleDOI
TL;DR: Long-term changes of PM sources at two megacities of Beijing and Nanjing indicated that the contributions of fossil fuel and industrial sources have been declining after stricter emission controls in recent years.

168 citations

Journal Article
TL;DR: The effects of air pollution on health have been generating attention for years as mentioned in this paper, and a large number of pulmonologists have recently expressed concerns about this in an open letter to Dutch Members of Parliament.
Abstract: The effects of air pollution on health have been generating attention for years. A large number of pulmonologists have recently expressed concerns about this in an open letter to Dutch Members of Parliament. Air pollution arises mainly in all kinds of combustion processes; in addition, atmospheric chemical reactions play a role in the formation of ozone and particulate matter. Health effects are both acute (increase in daily mortality and morbidity after days with increased concentrations of air pollution) as well as chronic (shortened life span and increased incidence of respiratory and cardiovascular diseases in areas with elevated concentrations of air pollution). These effects already occur at concentrations that are clearly lower than those currently observed in the Netherlands.

106 citations

Journal ArticleDOI
TL;DR: This study showed that particles from crop residue and apple wood combustion were mainly organic matter (OM) in smoldering phase, whereas soot-OM internally mixed with K in flaming phase, which is important to document properties of primary particles from combustion sources, which can be used to trace the sources of ambient particles.
Abstract: Morphology, composition, and mixing state of individual particles emitted from crop residue, wood, and solid waste combustion in a residential stove were analyzed using transmission electron microscopy (TEM). Our study showed that particles from crop residue and apple wood combustion were mainly organic matter (OM) in smoldering phase, whereas soot-OM internally mixed with K in flaming phase. Wild grass combustion in flaming phase released some Cl-rich-OM/soot particles and cardboard combustion released OM and S-rich particles. Interestingly, particles from hardwood (pear wood and bamboo) and softwood (cypress and pine wood) combustion were mainly soot and OM in the flaming phase, respectively. The combustion of foam boxes, rubber tires, and plastic bottles/bags in the flaming phase released large amounts of soot internally mixed with a small amount of OM, whereas the combustion of printed circuit boards and copper-core cables emitted large amounts of OM with Br-rich inclusions. In addition, the printed circuit board combustion released toxic metals containing Pb, Zn, Sn, and Sb. The results are important to document properties of primary particles from combustion sources, which can be used to trace the sources of ambient particles and to know their potential impacts in human health and radiative forcing in the air.

83 citations

Journal ArticleDOI
TL;DR: In this article, the authors investigate the sources of organic carbon (OC) and elemental carbon (EC) in Xi'an, China, based on 1-year radiocarbon and stable carbon isotope measurements.
Abstract: . Sources of organic carbon (OC) and elemental carbon (EC) in Xi'an, China, are investigated based on 1-year radiocarbon and stable carbon isotope measurements. The radiocarbon results demonstrate that EC is dominated by fossil sources throughout the year, with a mean contribution of 83±5 % ( 7±2 µg m−3 ). The remaining 17±5 % ( 1.5±1 µg m−3 ) is attributed to biomass burning, with a higher contribution in the winter ( ∼24 %) compared to the summer ( ∼14 %). Stable carbon isotopes of EC ( δ13CEC ) are enriched in winter ( - 23.2 ± 0.4 ‰) and depleted in summer ( - 25.9 ± 0.5 ‰), indicating the influence of coal combustion in winter and liquid fossil fuel combustion in summer. By combining radiocarbon and stable carbon signatures, relative contributions from coal combustion and liquid fossil fuel combustion are estimated to be 45 % (median; 29 %–58 %, interquartile range) and 31 % (18 %–46 %) in winter, respectively, whereas in other seasons more than one half of EC is from liquid fossil combustion. In contrast with EC, the contribution of non-fossil sources to OC is much larger, with an annual average of 54±8 % ( 12±10 µg m−3 ). Clear seasonal variations are seen in OC concentrations both from fossil and non-fossil sources, with maxima in winter and minima in summer because of unfavorable meteorological conditions coupled with enhanced fossil and non-fossil activities in winter, mainly biomass burning and domestic coal burning. δ13COC exhibited similar values to δ13CEC , and showed strong correlations ( r2=0.90 ) in summer and autumn, indicating similar source mixtures with EC. In spring, δ13COC is depleted (1.1 ‰–2.4 ‰) compared to δ13CEC , indicating the importance of secondary formation of OC (e.g., from volatile organic compound precursors) in addition to primary sources. Modeled mass concentrations and source contributions of primary OC are compared to the measured mass and source contributions. There is strong evidence that both secondary formation and photochemical loss processes influence the final OC concentrations.

62 citations


Cites background from "The importance of non-fossil source..."

  • ...Comparable annual ffossil(EC) was reported at an urban site of Beijing (79 ± 6% (Zhang et al., 2015b); 82 ± 7% (Zhang et al., 2017)) and a background receptor site of Ningbo (77 ± 15% (Liu et al., 2013))....

    [...]

Journal ArticleDOI
TL;DR: A ubiquity and dominance of nonfossil contribution to OC aerosols is identified not only in rural/background/remote regions but also in urban regions, which may be explained by cooking contributions, regional transportation or local emissions of seasonal-dependent biomass burning emission.
Abstract: Source apportionment of organic carbon (OC) and elemental carbon (EC) from PM1 (particulate matter with a diameter equal to or smaller than 1 μm) in Beijing, China was carried out using radiocarbon (14C) measurement. Despite a dominant fossil-fuel contribution to EC due to large emissions from traffic and coal combustion, nonfossil sources are dominant contributors of OC in Beijing throughout the year except during the winter. Primary emission was the most important contributor to fossil-fuel derived OC for all seasons. A clear seasonal trend was found for biomass-burning contribution to OC with the highest in autumn and spring, followed by winter and summer. 14C results were also integrated with those from positive matrix factorization (PMF) of organic aerosols from aerosol mass spectrometer (AMS) measurements during winter and spring. The results suggest that the fossil-derived primary OC was dominated by coal combustion emissions whereas secondary OC was mostly from fossil-fuel emissions. Taken together with previous 14C studies in Asia, Europe and USA, a ubiquity and dominance of nonfossil contribution to OC aerosols is identified not only in rural/background/remote regions but also in urban regions, which may be explained by cooking contributions, regional transportation or local emissions of seasonal-dependent biomass burning emission. In addition, biogenic and biomass burning derived SOA may be further enhanced by unresolved atmospheric processes.

59 citations

References
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Journal ArticleDOI
TL;DR: In spite of considerable progress in recent years, a quantitative and predictive understanding of atmospheric aerosol sources, chemical composition, transformation processes and environmental effects is still rather limited, and therefore represents a major research challenge in atmospheric science as discussed by the authors.

325 citations


"The importance of non-fossil source..." refers background in this paper

  • ...Ambient OC is a mixture of primary organic carbon (POC), which is emitted from various combustion processes, and secondary organic carbon (SOC), which is formed through the oxidation of volatile organic compounds (VOCs) (Pöschl, 2005; Calvo et al., 2013)....

    [...]

  • ...4 (POC), which is emitted from various combustion processes, and secondary organic carbon (SOC), which is formed through the oxidation of volatile organic compounds (VOCs) (Pöschl, 2005; Calvo et al., 2013)....

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01 Feb 2010-Tellus B
TL;DR: In this paper, high-precision atmospheric Δ 14 CO 2 records covering the last two decades are presented, and evaluated in terms of changing (radio)carbon sources and sinks, using the coarse-grid carbon cycle model GRACE.
Abstract: Global high-precision atmospheric Δ 14 CO 2 records covering the last two decades are presented, and evaluated in terms of changing (radio)carbon sources and sinks, using the coarse-grid carbon cycle model GRACE. Dedicated simulations of global trends and interhemispheric differences with respect to atmospheric CO 2 as well as δ 13 CO 2 and Δ 14 CO 2 , are shown to be in good agreement with the available observations (1940–2008). While until the 1990s the decreasing trend of Δ 14 CO 2 was governed by equilibration of the atmospheric bomb 14 C perturbation with the oceans and terrestrial biosphere, the largest perturbation today are emissions of 14 C-free fossil fuel CO 2 . This source presently depletes global atmospheric Δ 14 CO 2 by 12–14‰ yr -1 , which is partially compensated by 14 CO 2 release from the biosphere, industrial 14 C emissions and natural 14 C production. Fossil fuel emissions also drive the changing north–south gradient, showing lower Δ 14 C in the northern hemisphere only since 2002. The fossil fuel-induced north–south (and also troposphere–stratosphere) Δ 14 CO 2 gradient today also drives the tropospheric Δ 14 CO 2 seasonality through variations of air mass exchange between these atmospheric compartments. Neither the observed temporal trend nor the Δ 14 CO 2 north–south gradient may constrain global fossil fuel CO 2 emissions to better than 25%, due to large uncertainties in other components of the (radio)carbon cycle.DOI: 10.1111/j.1600-0889.2009.00446.x

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TL;DR: In this paper, a long-term trend of visibility in Guangzhou (one of the largest cities in PRD) shows that between 1954 and 2006, there is a rapid change in visibility.

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Additional excerpts

  • ...5 loading can cause a reduction in visibility, climate changes, and human respiratory-cardiovascular diseases (Brunekreef and Holgate, 2002; Menon et al., 2002; Deng et al., 2008; Wang et al., 2014b), many concerns were raised by the public, government, and scientists....

    [...]

Journal ArticleDOI
TL;DR: It was estimated that 1957 Gg of BC were emitted in China in 2007, which is greater than previously reported, and spatial bias in province-level disaggregation was reduced, mainly due to uneven per capita emissions within provinces.
Abstract: Black carbon (BC) emissions from China are of global concern. A new BC emission inventory (PKU-BC(China)) has been developed with the following improvements: (1) The emission factor database was updated; (2) a 0.1° × 0.1° gridded map was produced for 2007 based on county-level proxies; (3) time trends were derived for 1949–2007 and predicted for 2008–2050; and (4) the uncertainties associated with the inventory were quantified. It was estimated that 1957 Gg of BC were emitted in China in 2007, which is greater than previously reported. Residential coal combustion was the largest source, followed by residential biofuel burning, coke production, diesel vehicles, and brick kilns. By using a county-level disaggregation method, spatial bias in province-level disaggregation, mainly due to uneven per capita emissions within provinces, was reduced by 42.5%. Emissions increased steadily since 1949 until leveling off in the mid-1990s, due to a series of technological advances and to socioeconomic progress. BC emiss...

255 citations


"The importance of non-fossil source..." refers background in this paper

  • ...…China), Guangdong (south China, the capital is Guangzhou), Shanxi (west China, the capital is Xi'an) and Hubei (central China, the capital is Wuhan), and the corresponding value for residential solid biomass is 880 Gg, 0 Gg, 22,000 Gg, 14,000 Gg and 26,000 Gg, respectively (Wang et al., 2012)....

    [...]

  • ...5 85,000 Gg, 80,000 Gg, 35,000 Gg, in Beijing (north China), Shanghai (east China), Guangdong (south China, the capital is Guangzhou), Shanxi (west China, the capital is Xi'an) and Hubei (central China, the capital is Wuhan), and the corresponding value for residential solid biomass is 880 Gg, 0 Gg, 22,000 Gg, 14,000 Gg and 26,000 Gg, respectively (Wang et al., 2012)....

    [...]

Journal ArticleDOI
TL;DR: The results show that these severe haze events were equally affected by biomass combustion in all three regions, whereas the sources of the dominant fossil fuel component was dramatically different between north and south.
Abstract: Thick haze plagued northeastern China in January 2013, strongly affecting both regional climate and human respiratory health. Here, we present dual carbon isotope constrained (Δ14C and δ13C) source apportionment for combustion-derived black carbon aerosol (BC) for three key hotspot regions (megacities): North China Plain (NCP, Beijing), the Yangtze River Delta (YRD, Shanghai), and the Pearl River Delta (PRD, Guangzhou) for January 2013. BC, here quantified as elemental carbon (EC), is one of the most health-detrimental components of PM2.5 and a strong climate warming agent. The results show that these severe haze events were equally affected (∼30%) by biomass combustion in all three regions, whereas the sources of the dominant fossil fuel component was dramatically different between north and south. In the NCP region, coal combustion accounted for 66% (46–74%, 95% C.I.) of the EC, whereas, in the YRD and PRD regions, liquid fossil fuel combustion (e.g., traffic) stood for 46% (18–66%) and 58% (38–68%), re...

223 citations

Related Papers (5)
Frequently Asked Questions (13)
Q1. What are the contributions in "The importance of non-fossil sources in carbonaceous aerosols in a megacity of central china during the 2013 winter haze episode: a source apportionment constrained by radiocarbon and organic tracers" ?

The importance of non-fossil sources in carbonaceous aerosols in a megacity of central China during the 2013 winter haze episode: A source apportionment constrained by radiocarbon and organic tracers Junwen Liu a, b, Jun Li a, *, Matthias Vonwiller b, c, Di Liu a, Hairong Cheng d, Kaijun Shen a, Gary Salazar b, Konstantinos Agrios b, c, Yanlin Zhang b, c, 1, Quanfu He a, Xiang Ding a, Guangcai Zhong a, Xinming Wang a, Sönke Szidat b, * *, Gan Zhang a a State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640, China b Department of Chemistry and Biochemistry & Oeschger Centre for Climate Change Research, University of Bern, Berne, 3012, Switzerland c Laboratory of Radiochemistry, Paul Scherrer Institute, Villigen-PSI, 5232, Switzerland d Department of Environmental Engineering, School of Resource and Environmental Science, Wuhan University, Wuhan, 430079, China * Corresponding author. 

Using an aerodyne aerosol chemical speciation monitor, Sun et al. (2014) found that stagnant meteorological conditions, coal combustion, secondary production, and regional transport were the main factors leading to the formation of this haze in Beijing. 

Because a high PM2.5 loading can cause a reduction in visibility, climate changes, and human respiratory-cardiovascular diseases (Brunekreef and Holgate, 2002; Menon et al., 2002; Deng et al., 2008; Wang et al., 2014b), many concerns were raised by the public, government, and scientists. 

These carbon particles in the atmosphere have two sources: fossil fuel (FF, e.g., from traffic exhaust, coal combustion, industry) and non-fossil (NF, e.g., from open/forest fire, biofuel burning, biogenic emission) emissions. 

A source-apportionment method for OC, including primary and secondary sources, was implemented using the measured carbon fractions, anhydrosugars, and 14C isotopic signals. 

According to the annual report of the Editorial Department of Wuhan Statistical Yearbook-2014, the gross domestic product was composed of agriculture (3.7%), industry (48.6%), and other sectors (47.7%). 

Andersson et al. (2015) found that during this haze period FF sources on average contributed 74%, 68% and 68% to EC in Beijing, Shanghai and Guangzhou, respectively. 

To determine the origins of haze particles, the authors measured 14C isotopic signals and unique organic tracers in PM2.5 samples with various levels in Wuhan (Fig. S1), the largest (~550 km2) and most densely populated metropolis (~10 million) in central China. 

Values of fm for WSOC and TC were calculated from the isotopic mass conservation, and the fm(OC) values reported here were corrected by a field blank (0.45 µg C/cm2; fm = 0.61 ± 0.02). 

These results suggest that biomass burning is an important driver for the haze phenomenon in Chinese cities, which probably because the burning of biofuel is still very extensive in China, especially in winter season. 

this large-scale haze crisis was very likely caused by the convergence of materials from numerous point sources in regions with different sources. 

These results show a significantly dominant influence of BB on OCnf_sec during this long-lasting winter haze, corresponding to the very low levels of biogenic VOCs in winter. 

In this study, a rough estimation of SOCbb (SOCbb = OCnf_sec - SOCbio) was obtained based on the combination of 14C and molecular markers of biogenic emissions (Table S2).