Alessandro Zanchetta, Linda M. J. Kooijmans, S. V. van Heuven, A. Scifo, H. Scheeren, I. Mammarella, U. Karstens, Jin Ma, M. Krol, Huilin Chen
{"title":"Sources and sinks of carbonyl sulfide inferred from tower and mobile atmospheric observations in the Netherlands","authors":"Alessandro Zanchetta, Linda M. J. Kooijmans, S. V. van Heuven, A. Scifo, H. Scheeren, I. Mammarella, U. Karstens, Jin Ma, M. Krol, Huilin Chen","doi":"10.5194/bg-20-3539-2023","DOIUrl":null,"url":null,"abstract":"Abstract. Carbonyl sulfide (COS) is a promising tracer for the estimation of\nterrestrial ecosystem gross primary production (GPP). However, understanding\nits non-GPP-related sources and sinks, e.g., anthropogenic sources and soil\nsources and sinks, is also critical to the success of the approach. Here we\ninfer the regional sources and sinks of COS using continuous in situ mole fraction\nprofile measurements of COS along the 60 m tall Lutjewad tower (1 m a.s.l.;\n53∘24′ N, 6∘21′ E) in the Netherlands. To identify\npotential sources that caused the observed enhancements of COS mole\nfractions at Lutjewad, both discrete flask samples and in situ measurements\nin the province of Groningen were made from a mobile van using a quantum\ncascade laser spectrometer (QCLS). We also simulated the COS mole fractions\nat Lutjewad using the Stochastic Time-Inverted Lagrangian Transport (STILT)\nmodel combined with emission inventories and plant uptake fluxes. We\ndetermined the nighttime COS fluxes to be -3.0±2.6 pmol m−2 s−1 using the radon-tracer correlation approach and Lutjewad\nobservations. Furthermore, we identified and quantified several COS sources,\nincluding biodigesters, sugar production facilities and silicon carbide\nproduction facilities in the province of Groningen. Moreover, the simulation\nresults show that the observed COS enhancements can be partially explained\nby known industrial sources of COS and CS2, in particular from the Ruhr\nValley (51.5∘ N, 7.2∘ E) and Antwerp (51.2∘ N,\n4.4∘ E) areas. The contribution of likely missing anthropogenic\nsources of COS and CS2 in the inventory may be significant. The impact\nof the identified sources in the province of Groningen is estimated to be\nnegligible in terms of the observed COS enhancements. However, in specific\nconditions, these sources may influence the measurements in Lutjewad. These\nresults are valuable for improving our understanding of the sources and\nsinks of COS, contributing to the use of COS as a tracer for GPP.\n","PeriodicalId":8899,"journal":{"name":"Biogeosciences","volume":" ","pages":""},"PeriodicalIF":3.9000,"publicationDate":"2023-08-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Biogeosciences","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.5194/bg-20-3539-2023","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ECOLOGY","Score":null,"Total":0}
引用次数: 0
Abstract
Abstract. Carbonyl sulfide (COS) is a promising tracer for the estimation of
terrestrial ecosystem gross primary production (GPP). However, understanding
its non-GPP-related sources and sinks, e.g., anthropogenic sources and soil
sources and sinks, is also critical to the success of the approach. Here we
infer the regional sources and sinks of COS using continuous in situ mole fraction
profile measurements of COS along the 60 m tall Lutjewad tower (1 m a.s.l.;
53∘24′ N, 6∘21′ E) in the Netherlands. To identify
potential sources that caused the observed enhancements of COS mole
fractions at Lutjewad, both discrete flask samples and in situ measurements
in the province of Groningen were made from a mobile van using a quantum
cascade laser spectrometer (QCLS). We also simulated the COS mole fractions
at Lutjewad using the Stochastic Time-Inverted Lagrangian Transport (STILT)
model combined with emission inventories and plant uptake fluxes. We
determined the nighttime COS fluxes to be -3.0±2.6 pmol m−2 s−1 using the radon-tracer correlation approach and Lutjewad
observations. Furthermore, we identified and quantified several COS sources,
including biodigesters, sugar production facilities and silicon carbide
production facilities in the province of Groningen. Moreover, the simulation
results show that the observed COS enhancements can be partially explained
by known industrial sources of COS and CS2, in particular from the Ruhr
Valley (51.5∘ N, 7.2∘ E) and Antwerp (51.2∘ N,
4.4∘ E) areas. The contribution of likely missing anthropogenic
sources of COS and CS2 in the inventory may be significant. The impact
of the identified sources in the province of Groningen is estimated to be
negligible in terms of the observed COS enhancements. However, in specific
conditions, these sources may influence the measurements in Lutjewad. These
results are valuable for improving our understanding of the sources and
sinks of COS, contributing to the use of COS as a tracer for GPP.
期刊介绍:
Biogeosciences (BG) is an international scientific journal dedicated to the publication and discussion of research articles, short communications and review papers on all aspects of the interactions between the biological, chemical and physical processes in terrestrial or extraterrestrial life with the geosphere, hydrosphere and atmosphere. The objective of the journal is to cut across the boundaries of established sciences and achieve an interdisciplinary view of these interactions. Experimental, conceptual and modelling approaches are welcome.