S.P Singh, G.S Satsangi, P Khare, A Lakhani, K Maharaj Kumari, S.S Srivastava
{"title":"大气氨的多相测量","authors":"S.P Singh, G.S Satsangi, P Khare, A Lakhani, K Maharaj Kumari, S.S Srivastava","doi":"10.1016/S1465-9972(00)00029-5","DOIUrl":null,"url":null,"abstract":"<div><p>Measurement of ammonia in vapour phase, particulate and rain was made at a suburban site of India. Vapour phase concentrations varied between 0.97 and 25.5 μg m<sup>−3</sup> (57.1–1500.0 nmol m<sup>−3</sup>) and diurnal variation study showed high concentration of NH<sub>3</sub> during night time and minimum at 0600 h (early morning). Particulate phase NH<sub>4</sub> values ranged between 1.2 and 5.3 μg m<sup>−3</sup> (66.7–294.4 nmol m<sup>−3</sup>). Dry deposition flux was determined from model calculations. Day time NH<sub>3</sub> flux was found to be 8.4±4.0 mg m<sup>−2</sup> d<sup>−1</sup> and that of night 2.2±1.2 mg m<sup>−2</sup> d<sup>−1</sup>. With respect to particulate deposition flux was found 0.2±0.1 mg m<sup>−2</sup> d<sup>−1</sup> while in precipitation values of NH<sub>4</sub> ranged between 0.7 and 74.4 μeq l<sup>−1</sup>. Regression analysis of ammonium concentration with rain volume and deposition indicates that NH<sub>3</sub> concentration is being controlled by both gas and particulate ammonium. Annual inputs for wet and dry deposition were found to be 0.34±0.3 and 3.9±1.9 g m<sup>−2</sup> y<sup>−1</sup>.</p></div>","PeriodicalId":100235,"journal":{"name":"Chemosphere - Global Change Science","volume":"3 1","pages":"Pages 107-116"},"PeriodicalIF":0.0000,"publicationDate":"2001-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S1465-9972(00)00029-5","citationCount":"42","resultStr":"{\"title\":\"Multiphase measurement of atmospheric ammonia\",\"authors\":\"S.P Singh, G.S Satsangi, P Khare, A Lakhani, K Maharaj Kumari, S.S Srivastava\",\"doi\":\"10.1016/S1465-9972(00)00029-5\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Measurement of ammonia in vapour phase, particulate and rain was made at a suburban site of India. Vapour phase concentrations varied between 0.97 and 25.5 μg m<sup>−3</sup> (57.1–1500.0 nmol m<sup>−3</sup>) and diurnal variation study showed high concentration of NH<sub>3</sub> during night time and minimum at 0600 h (early morning). Particulate phase NH<sub>4</sub> values ranged between 1.2 and 5.3 μg m<sup>−3</sup> (66.7–294.4 nmol m<sup>−3</sup>). Dry deposition flux was determined from model calculations. Day time NH<sub>3</sub> flux was found to be 8.4±4.0 mg m<sup>−2</sup> d<sup>−1</sup> and that of night 2.2±1.2 mg m<sup>−2</sup> d<sup>−1</sup>. With respect to particulate deposition flux was found 0.2±0.1 mg m<sup>−2</sup> d<sup>−1</sup> while in precipitation values of NH<sub>4</sub> ranged between 0.7 and 74.4 μeq l<sup>−1</sup>. Regression analysis of ammonium concentration with rain volume and deposition indicates that NH<sub>3</sub> concentration is being controlled by both gas and particulate ammonium. Annual inputs for wet and dry deposition were found to be 0.34±0.3 and 3.9±1.9 g m<sup>−2</sup> y<sup>−1</sup>.</p></div>\",\"PeriodicalId\":100235,\"journal\":{\"name\":\"Chemosphere - Global Change Science\",\"volume\":\"3 1\",\"pages\":\"Pages 107-116\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2001-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/S1465-9972(00)00029-5\",\"citationCount\":\"42\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Chemosphere - Global Change Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1465997200000295\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemosphere - Global Change Science","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1465997200000295","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Measurement of ammonia in vapour phase, particulate and rain was made at a suburban site of India. Vapour phase concentrations varied between 0.97 and 25.5 μg m−3 (57.1–1500.0 nmol m−3) and diurnal variation study showed high concentration of NH3 during night time and minimum at 0600 h (early morning). Particulate phase NH4 values ranged between 1.2 and 5.3 μg m−3 (66.7–294.4 nmol m−3). Dry deposition flux was determined from model calculations. Day time NH3 flux was found to be 8.4±4.0 mg m−2 d−1 and that of night 2.2±1.2 mg m−2 d−1. With respect to particulate deposition flux was found 0.2±0.1 mg m−2 d−1 while in precipitation values of NH4 ranged between 0.7 and 74.4 μeq l−1. Regression analysis of ammonium concentration with rain volume and deposition indicates that NH3 concentration is being controlled by both gas and particulate ammonium. Annual inputs for wet and dry deposition were found to be 0.34±0.3 and 3.9±1.9 g m−2 y−1.