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

Hydrologic dynamics control dissolve...

Bellmore, Rebecca Anne.

FindBook

Google Book

Amazon

博客來

Hydrologic dynamics control dissolved organic matter export from watersheds: Fields-scale processes in a small, artificially drained agricultural catchment, and patterns across ecosystems.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Hydrologic dynamics control dissolved organic matter export from watersheds: Fields-scale processes in a small, artificially drained agricultural catchment, and patterns across ecosystems./
作者:	Bellmore, Rebecca Anne.
面頁冊數:	268 p.
附註:	Source: Dissertation Abstracts International, Volume: 76-07(E), Section: B.
Contained By:	Dissertation Abstracts International76-07B(E).
標題:	Environmental Sciences. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3684751
ISBN:	9781321601268

Hydrologic dynamics control dissolved organic matter export from watersheds: Fields-scale processes in a small, artificially drained agricultural catchment, and patterns across ecosystems.
Bellmore, Rebecca Anne.

Hydrologic dynamics control dissolved organic matter export from watersheds: Fields-scale processes in a small, artificially drained agricultural catchment, and patterns across ecosystems. - 268 p.

Source: Dissertation Abstracts International, Volume: 76-07(E), Section: B.

Thesis (Ph.D.)--Washington State University, 2014.

This item must not be sold to any third party vendors.

Dissolved organic matter (DOM) is an important component of nutrient cycling and energy transfer within and between ecosystems. Understanding controls over the magnitude and quality of DOM that is transferred from soils to surface water is needed to better characterize the terrestrial-aquatic carbon flux and effects of terrestrial DOM on downstream ecosystems. A meta-analysis of the response of in-stream dissolved organic nitrogen concentration (DON) to high flow events indicates that DON typically increases with flow across a wide range of ecosystem types, likely as novel DOM sources in the landscape are mobilized and transported to streams and rivers. Mechanisms controlling DOM export, including dissolved organic carbon (DOC) and DON concentrations and the quality of DOM, were examined in a small agricultural catchment in eastern Washington State. In the soil column, DOC concentration declined and source of DOM shifted from humic-like and plant-derived to microbially-derived with depth through the profile. Across seasons and years, DOM exported via drain discharge during low flows resembled that found deep in the soil profile, and DOM exported during high flows suggests topsoil and litter sources contribute to export. A simple mixing model suggests that litter leachate can contribute over 50% of DOM during peak flow. Based on modeled contributions of litter, topsoil and subsoil DOM during storm events, DOC concentration is over-predicted, except for peak flows, suggesting removal via sorption and/or microbial decomposition in the soil column control DOC export on the timescale of events. Although the character of exported DOM shifts with flow conditions, laboratory incubations suggest bioavailability to the stream sediment microbial community is consistently low, with a maximum of 7% loss over 6 days, indicating exported DOM is likely transported beyond the immediate stream reach. An analysis of anticipated effects of climate change on the flow regime in the catchment projects the wettest years to become more variable, with non-linear effects on the magnitude of DOC export. Finally I explore how climate change assessments can be incorporated into nonpoint source nutrient management plans, despite current uncertainty about the magnitude and timeframe of climate effects on nutrient loading.

ISBN: 9781321601268Subjects--Topical Terms:

676987
Environmental Sciences.

Hydrologic dynamics control dissolved organic matter export from watersheds: Fields-scale processes in a small, artificially drained agricultural catchment, and patterns across ecosystems.
LDR:03413nmm a2200301 4500 001 2057614
005 20150630115552.5
008 170521s2014 ||||||||||||||||| ||eng d
020 $a 9781321601268
035 $a (MiAaPQ)AAI3684751
035 $a AAI3684751
040 $a MiAaPQ $c MiAaPQ
100 1 $a Bellmore, Rebecca Anne. $3 3171484
245 1 0 $a Hydrologic dynamics control dissolved organic matter export from watersheds: Fields-scale processes in a small, artificially drained agricultural catchment, and patterns across ecosystems.
300 $a 268 p.
500 $a Source: Dissertation Abstracts International, Volume: 76-07(E), Section: B.
500 $a Adviser: John A. Harrison.
502 $a Thesis (Ph.D.)--Washington State University, 2014.
506 $a This item must not be sold to any third party vendors.
520 $a Dissolved organic matter (DOM) is an important component of nutrient cycling and energy transfer within and between ecosystems. Understanding controls over the magnitude and quality of DOM that is transferred from soils to surface water is needed to better characterize the terrestrial-aquatic carbon flux and effects of terrestrial DOM on downstream ecosystems. A meta-analysis of the response of in-stream dissolved organic nitrogen concentration (DON) to high flow events indicates that DON typically increases with flow across a wide range of ecosystem types, likely as novel DOM sources in the landscape are mobilized and transported to streams and rivers. Mechanisms controlling DOM export, including dissolved organic carbon (DOC) and DON concentrations and the quality of DOM, were examined in a small agricultural catchment in eastern Washington State. In the soil column, DOC concentration declined and source of DOM shifted from humic-like and plant-derived to microbially-derived with depth through the profile. Across seasons and years, DOM exported via drain discharge during low flows resembled that found deep in the soil profile, and DOM exported during high flows suggests topsoil and litter sources contribute to export. A simple mixing model suggests that litter leachate can contribute over 50% of DOM during peak flow. Based on modeled contributions of litter, topsoil and subsoil DOM during storm events, DOC concentration is over-predicted, except for peak flows, suggesting removal via sorption and/or microbial decomposition in the soil column control DOC export on the timescale of events. Although the character of exported DOM shifts with flow conditions, laboratory incubations suggest bioavailability to the stream sediment microbial community is consistently low, with a maximum of 7% loss over 6 days, indicating exported DOM is likely transported beyond the immediate stream reach. An analysis of anticipated effects of climate change on the flow regime in the catchment projects the wettest years to become more variable, with non-linear effects on the magnitude of DOC export. Finally I explore how climate change assessments can be incorporated into nonpoint source nutrient management plans, despite current uncertainty about the magnitude and timeframe of climate effects on nutrient loading.
590 $a School code: 0251.
650 4 $a Environmental Sciences. $3 676987
650 4 $a Biogeochemistry. $3 545717
650 4 $a Water Resource Management. $3 1669219
690 $a 0768
690 $a 0425
690 $a 0595
710 2 $a Washington State University. $b Environmental and Natural Resource Sciences. $3 2105128
773 0 $t Dissertation Abstracts International $g 76-07B(E).
790 $a 0251
791 $a Ph.D.
792 $a 2014
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3684751