{"title":"浓度垂直剖面的σZ和H计算","authors":"J. Halitsky","doi":"10.1080/00022470.1986.10466187","DOIUrl":null,"url":null,"abstract":"In extracting Gaussian plume parameters from transverse profiles of concentration measured in model or full-scale tests of dispersion from an elevated source, a common practice is to employ a statistical best-fit procedure in conjunction with the general equation. This involves 1) a calculation of x by Equation 1 for each data point (y,z) using known parameter Q and combinations of assumed parameters sigma/sub y/, sigma/sub z/, u and H; 2) a comparison of calculated and observed values of x; and 3) minimization of the discrepancy for the complete data set.","PeriodicalId":17188,"journal":{"name":"Journal of the Air Pollution Control Association","volume":"31 1","pages":"1357-1359"},"PeriodicalIF":0.0000,"publicationDate":"1986-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Calculation of σZ and H for an observed vertical profile of concentration\",\"authors\":\"J. Halitsky\",\"doi\":\"10.1080/00022470.1986.10466187\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In extracting Gaussian plume parameters from transverse profiles of concentration measured in model or full-scale tests of dispersion from an elevated source, a common practice is to employ a statistical best-fit procedure in conjunction with the general equation. This involves 1) a calculation of x by Equation 1 for each data point (y,z) using known parameter Q and combinations of assumed parameters sigma/sub y/, sigma/sub z/, u and H; 2) a comparison of calculated and observed values of x; and 3) minimization of the discrepancy for the complete data set.\",\"PeriodicalId\":17188,\"journal\":{\"name\":\"Journal of the Air Pollution Control Association\",\"volume\":\"31 1\",\"pages\":\"1357-1359\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1986-12-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of the Air Pollution Control Association\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1080/00022470.1986.10466187\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of the Air Pollution Control Association","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/00022470.1986.10466187","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Calculation of σZ and H for an observed vertical profile of concentration
In extracting Gaussian plume parameters from transverse profiles of concentration measured in model or full-scale tests of dispersion from an elevated source, a common practice is to employ a statistical best-fit procedure in conjunction with the general equation. This involves 1) a calculation of x by Equation 1 for each data point (y,z) using known parameter Q and combinations of assumed parameters sigma/sub y/, sigma/sub z/, u and H; 2) a comparison of calculated and observed values of x; and 3) minimization of the discrepancy for the complete data set.
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