{"title":"来自农业用水系统的氧化亚氮被高氮污染","authors":"Kiyo Hasegawa , Keisuke Hanaki , Tomonori Matsuo , Shin Hidaka","doi":"10.1016/S1465-9972(00)00009-X","DOIUrl":null,"url":null,"abstract":"<div><p>The agricultural water system especially contaminated with high nitrogen was surveyed in Saitama Prefecture, Japan. The anthropogenic nitrogen, such as fertilizer, livestock wastes, etc., caused the occurrence of high nitrate-nitrogen (20–30 mgN/l) in the groundwater in this area. The concentration of dissolved N<sub>2</sub>O in the groundwater ranged from 0 to 28.2 μgN/l. The main source of N<sub>2</sub>O in the groundwater seemed to be nitrified N from the stockbreeding areas. As this groundwater flowed into the organic matter rich areas, such as paddy fields and a small river, denitrification actively occurred and much N<sub>2</sub>O was produced there. Dissolved N<sub>2</sub>O concentration in these places ranged from 10 to 400 μgN/l and N<sub>2</sub>O gas flux from the small river was extremely high (about 500 μgN/m<sup>2</sup> <!-->·<!--> <!-->min). While nitrate-nitrogen could be removed in these areas, these areas often served as significant N<sub>2</sub>O sources. The effective and feasible method to decrease the N<sub>2</sub>O emission ratio while keeping the denitrification activity high should be explored.</p><p>To demonstrate the efficiency of putting sulfur into soil as a denitrification electron donor, the column and the batch experiments were carried out. When denitrification proceeded sufficiently, N<sub>2</sub>O formation in the soil column packed with elemental sulfur was kept low. In the case of adding CaCO<sub>3</sub> for pH adjustment and adding elemental sulfur or iron sulfide, N<sub>2</sub>O production was suppressed. This indicated the possibility to decrease N<sub>2</sub>O emission by adding sulfur into the soil and proceeding sulfur denitrification.</p></div>","PeriodicalId":100235,"journal":{"name":"Chemosphere - Global Change Science","volume":"2 3","pages":"Pages 335-345"},"PeriodicalIF":0.0000,"publicationDate":"2000-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S1465-9972(00)00009-X","citationCount":"63","resultStr":"{\"title\":\"Nitrous oxide from the agricultural water system contaminated with high nitrogen\",\"authors\":\"Kiyo Hasegawa , Keisuke Hanaki , Tomonori Matsuo , Shin Hidaka\",\"doi\":\"10.1016/S1465-9972(00)00009-X\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The agricultural water system especially contaminated with high nitrogen was surveyed in Saitama Prefecture, Japan. The anthropogenic nitrogen, such as fertilizer, livestock wastes, etc., caused the occurrence of high nitrate-nitrogen (20–30 mgN/l) in the groundwater in this area. The concentration of dissolved N<sub>2</sub>O in the groundwater ranged from 0 to 28.2 μgN/l. The main source of N<sub>2</sub>O in the groundwater seemed to be nitrified N from the stockbreeding areas. As this groundwater flowed into the organic matter rich areas, such as paddy fields and a small river, denitrification actively occurred and much N<sub>2</sub>O was produced there. Dissolved N<sub>2</sub>O concentration in these places ranged from 10 to 400 μgN/l and N<sub>2</sub>O gas flux from the small river was extremely high (about 500 μgN/m<sup>2</sup> <!-->·<!--> <!-->min). While nitrate-nitrogen could be removed in these areas, these areas often served as significant N<sub>2</sub>O sources. The effective and feasible method to decrease the N<sub>2</sub>O emission ratio while keeping the denitrification activity high should be explored.</p><p>To demonstrate the efficiency of putting sulfur into soil as a denitrification electron donor, the column and the batch experiments were carried out. When denitrification proceeded sufficiently, N<sub>2</sub>O formation in the soil column packed with elemental sulfur was kept low. In the case of adding CaCO<sub>3</sub> for pH adjustment and adding elemental sulfur or iron sulfide, N<sub>2</sub>O production was suppressed. This indicated the possibility to decrease N<sub>2</sub>O emission by adding sulfur into the soil and proceeding sulfur denitrification.</p></div>\",\"PeriodicalId\":100235,\"journal\":{\"name\":\"Chemosphere - Global Change Science\",\"volume\":\"2 3\",\"pages\":\"Pages 335-345\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2000-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/S1465-9972(00)00009-X\",\"citationCount\":\"63\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Chemosphere - Global Change Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S146599720000009X\",\"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/S146599720000009X","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Nitrous oxide from the agricultural water system contaminated with high nitrogen
The agricultural water system especially contaminated with high nitrogen was surveyed in Saitama Prefecture, Japan. The anthropogenic nitrogen, such as fertilizer, livestock wastes, etc., caused the occurrence of high nitrate-nitrogen (20–30 mgN/l) in the groundwater in this area. The concentration of dissolved N2O in the groundwater ranged from 0 to 28.2 μgN/l. The main source of N2O in the groundwater seemed to be nitrified N from the stockbreeding areas. As this groundwater flowed into the organic matter rich areas, such as paddy fields and a small river, denitrification actively occurred and much N2O was produced there. Dissolved N2O concentration in these places ranged from 10 to 400 μgN/l and N2O gas flux from the small river was extremely high (about 500 μgN/m2 · min). While nitrate-nitrogen could be removed in these areas, these areas often served as significant N2O sources. The effective and feasible method to decrease the N2O emission ratio while keeping the denitrification activity high should be explored.
To demonstrate the efficiency of putting sulfur into soil as a denitrification electron donor, the column and the batch experiments were carried out. When denitrification proceeded sufficiently, N2O formation in the soil column packed with elemental sulfur was kept low. In the case of adding CaCO3 for pH adjustment and adding elemental sulfur or iron sulfide, N2O production was suppressed. This indicated the possibility to decrease N2O emission by adding sulfur into the soil and proceeding sulfur denitrification.