Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/33458
DC FieldValueLanguage
dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorWang, W-
dc.creatorWang, T-
dc.date.accessioned2014-12-31T08:02:37Z-
dc.date.available2014-12-31T08:02:37Z-
dc.identifier.issn1352-2310-
dc.identifier.urihttp://hdl.handle.net/10397/33458-
dc.language.isoenen_US
dc.publisherPergamon Pressen_US
dc.subjectAerosol buffering capacityen_US
dc.subjectAtmospheric dispersionen_US
dc.subjectEmissionen_US
dc.subjectSO2 and NO(χ)en_US
dc.subjectSoil pHen_US
dc.titleOn acid rain formation in Chinaen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage4091-
dc.identifier.epage4093-
dc.identifier.volume30-
dc.identifier.issue23-
dc.identifier.doi10.1016/1352-2310(96)00115-X-
dcterms.bibliographicCitationAtmospheric environment, 1996, v. 30, no. 23, p. 4091-4093-
dcterms.isPartOfAtmospheric environment-
dcterms.issued1996-
dc.identifier.isiWOS:A1996VK13800017-
dc.identifier.scopus2-s2.0-0030306992-
dc.identifier.eissn1873-2844-
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