東華大學圖書館 |

語系: 繁體中文

說明(常見問題)

回圖書館首頁

手機版館藏查詢

登入

回首頁

切換: 標籤 | MARC模式 | ISBD

Formation of Secondary Organic Aeros...

El-Sayed, Marwa Mohamed Hosni Abdel Azim.

FindBook

Google Book

Amazon

博客來

Formation of Secondary Organic Aerosols in Atmospheric Liquid Water.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Formation of Secondary Organic Aerosols in Atmospheric Liquid Water./
作者:	El-Sayed, Marwa Mohamed Hosni Abdel Azim.
出版者:	Ann Arbor : ProQuest Dissertations & Theses, : 2018,
面頁冊數:	374 p.
附註:	Source: Dissertation Abstracts International, Volume: 79-10(E), Section: B.
Contained By:	Dissertation Abstracts International79-10B(E).
標題:	Atmospheric chemistry. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10745511
ISBN:	9780355989892

Formation of Secondary Organic Aerosols in Atmospheric Liquid Water.
El-Sayed, Marwa Mohamed Hosni Abdel Azim.

Formation of Secondary Organic Aerosols in Atmospheric Liquid Water. - Ann Arbor : ProQuest Dissertations & Theses, 2018 - 374 p.

Source: Dissertation Abstracts International, Volume: 79-10(E), Section: B.

Thesis (Ph.D.)--University of Maryland, Baltimore County, 2018.

The formation of secondary organic aerosols through aqueous processes (aqSOA) has been identified as an important route in forming organic aerosols; however, many aspects of this formation are still uncertain. One main uncertainty is the nature by which these aqueous compounds are formed, whether the formation is reversible, irreversible, or a mixture of both. To date, there are no ambient measurements to quantify or constrain the relative contributions of reversible/irreversible aqSOA. Hence, we have developed an online method to simultaneously measure water-soluble organic carbon in the gas (WSOCg) and particle (WSOC p) phases to characterize the reversible and irreversible uptake of water-soluble organic gases to aerosol liquid water (ALW) across the different seasons in Maryland located in the eastern United States.

ISBN: 9780355989892Subjects--Topical Terms:

544140
Atmospheric chemistry.

Formation of Secondary Organic Aerosols in Atmospheric Liquid Water.
LDR:03309nmm a2200325 4500 001 2201939
005 20190503113352.5
008 201008s2018 ||||||||||||||||| ||eng d
020 $a 9780355989892
035 $a (MiAaPQ)AAI10745511
035 $a (MiAaPQ)umbc:11793
035 $a AAI10745511
040 $a MiAaPQ $c MiAaPQ
100 1 $a El-Sayed, Marwa Mohamed Hosni Abdel Azim. $3 3428689
245 1 0 $a Formation of Secondary Organic Aerosols in Atmospheric Liquid Water.
260 1 $a Ann Arbor : $b ProQuest Dissertations & Theses, $c 2018
300 $a 374 p.
500 $a Source: Dissertation Abstracts International, Volume: 79-10(E), Section: B.
500 $a Adviser: Christopher J. Hennigan.
502 $a Thesis (Ph.D.)--University of Maryland, Baltimore County, 2018.
520 $a The formation of secondary organic aerosols through aqueous processes (aqSOA) has been identified as an important route in forming organic aerosols; however, many aspects of this formation are still uncertain. One main uncertainty is the nature by which these aqueous compounds are formed, whether the formation is reversible, irreversible, or a mixture of both. To date, there are no ambient measurements to quantify or constrain the relative contributions of reversible/irreversible aqSOA. Hence, we have developed an online method to simultaneously measure water-soluble organic carbon in the gas (WSOCg) and particle (WSOC p) phases to characterize the reversible and irreversible uptake of water-soluble organic gases to aerosol liquid water (ALW) across the different seasons in Maryland located in the eastern United States.
520 $a The formation of aqSOA was observed in all four seasons during the night, and was predominantly associated with the availability of ALW. In the fall and winter, there was no statistically significant difference in WSOC p concentrations through the dry and ambient channels, suggesting irreversible aqSOA formation. However, there was a systematic difference between ambient and dry WSOCp measurements in the late spring and summer, indicating reversible aqSOA formation. Conditions that promote reversible aqSOA formation were clearly present starting from the late spring and into the summer, but were not significant during the winter and the fall. During the late spring and summer, aqSOA formation was tightly linked with isoprene oxidation, while the aqSOA formed in the winter was associated with biomass burning due to residential heating. The quantity of evaporated WSOCp was strongly related to relative humidity, WSOCp concentrations, and NO x/isoprene ratios. The split between reversible and irreversible aqSOA formation was related to NOx, suggesting that low-NOx isoprene oxidation products were responsible for the reversible aqSOA. Given the diverse climatology and aerosol sources that impact Baltimore, it is likely that this phenomenon occurs in many other locations. The results presented in this thesis have several important implications for atmospheric chemistry, atmospheric modeling, several atmospheric measurement methods, and regulations and health.
590 $a School code: 0434.
650 4 $a Atmospheric chemistry. $3 544140
650 4 $a Environmental engineering. $3 548583
650 4 $a Chemical engineering. $3 560457
690 $a 0371
690 $a 0775
690 $a 0542
710 2 $a University of Maryland, Baltimore County. $b Engineering, Chemical and Biochemical. $3 1669092
773 0 $t Dissertation Abstracts International $g 79-10B(E).
790 $a 0434
791 $a Ph.D.
792 $a 2018
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10745511