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

Fire, Charcoal, and the Biogeochemis...

Pingree, Melissa Rose Ann.

FindBook

Google Book

Amazon

博客來

Fire, Charcoal, and the Biogeochemistry of Carbon and Nitrogen in Pacific Northwest Forest Soils.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Fire, Charcoal, and the Biogeochemistry of Carbon and Nitrogen in Pacific Northwest Forest Soils./
作者:	Pingree, Melissa Rose Ann.
出版者:	Ann Arbor : ProQuest Dissertations & Theses, : 2017,
面頁冊數:	152 p.
附註:	Source: Dissertation Abstracts International, Volume: 78-09(E), Section: B.
Contained By:	Dissertation Abstracts International78-09B(E).
標題:	Soil sciences. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10257267
ISBN:	9781369693492

Fire, Charcoal, and the Biogeochemistry of Carbon and Nitrogen in Pacific Northwest Forest Soils.
Pingree, Melissa Rose Ann.

Fire, Charcoal, and the Biogeochemistry of Carbon and Nitrogen in Pacific Northwest Forest Soils. - Ann Arbor : ProQuest Dissertations & Theses, 2017 - 152 p.

Source: Dissertation Abstracts International, Volume: 78-09(E), Section: B.

Thesis (Ph.D.)--University of Washington, 2017.

The rain shadow forests of the Olympic peninsula represent a unique, mixed-severity fire regime class in the midst of a highly productive landscape where spatial heterogeneity of fire severity may have significant implications for below and aboveground post-fire recovery. The purpose of this study was to quantify the impacts of wildfire on forest carbon (C) and nitrogen (N) pools and assess the influence of charcoal in a mixed-severity ecosystem on the Olympic Peninsula, Washington, USA. We established a fire chronosequence in forest stands ranging in time since fire (TSF) from 3 to 115 years prior to site establishment. At each site, we measured vegetation abundance, overstory composition, and attributes of surface mineral soil to a depth of 10 cm and forest floor organic matter that included pH, texture, bulk density, and C and N pools (dissolved organic C [DOC], phenol, ammonium, nitrate). Non-ionic resin lysimeters were buried at the interface of organic and mineral soil to measure the O-horizon leached DOC that would contact charcoal particles on the forest floor. Charcoal particles collected from the chronosequence sites were used in adsorption batch experimentation with phenol as a sorbate and measured an average 29.70 (+/- 6.23) mug phenol mg charcoal -1 adsorption capacity, which did not differ significantly between chronosequence sites. Wildfire-produced charcoal along the chronosequence showed high variability in adsorption capacity, which was partially explained by the thermogravimetric region of volatilized adsorbed compounds onto charcoal surfaces. The O-horizon leachate averaged 1.05 (SD +/- 2.87) g DOC m-2 year-1 and increased significantly along the TSF gradient (Pearson's r = 0.52; p < 0.0001). Multivariate, non-parametric analysis of soil and vegetation factors showed a significant relationship with the time since fire gradient between sites (p-value < 0.01) but not within sites. The TSF gradient was significantly correlated to charcoal mass in the O-horizon (r = -0.4), O-horizon C (r = 0.4), phenolic content in both O-horizon (r = 0.4) and mineral soils (r = 0.2), and potentially mineralizable N ( r = 0.4). Recent sites contained higher mineral soil total N and inorganic available N, though not significantly correlated with the TSF gradient. Over time, soils appear to shift toward phenolic-rich organic and mineral soils, higher moss cover, and a higher potentially mineralizable nitrogen index. This study provides evidence of a multivariate, belowground soil response that is less sensitive to wildfire disturbances than the aboveground vegetation.

ISBN: 9781369693492Subjects--Topical Terms:

2122699
Soil sciences.

Fire, Charcoal, and the Biogeochemistry of Carbon and Nitrogen in Pacific Northwest Forest Soils.
LDR:03608nmm a2200313 4500 001 2154750
005 20180419121556.5
008 190424s2017 ||||||||||||||||| ||eng d
020 $a 9781369693492
035 $a (MiAaPQ)AAI10257267
035 $a (MiAaPQ)washington:16830
035 $a AAI10257267
040 $a MiAaPQ $c MiAaPQ
100 1 $a Pingree, Melissa Rose Ann. $3 3342480
245 1 0 $a Fire, Charcoal, and the Biogeochemistry of Carbon and Nitrogen in Pacific Northwest Forest Soils.
260 1 $a Ann Arbor : $b ProQuest Dissertations & Theses, $c 2017
300 $a 152 p.
500 $a Source: Dissertation Abstracts International, Volume: 78-09(E), Section: B.
500 $a Adviser: Thomas H. DeLuca.
502 $a Thesis (Ph.D.)--University of Washington, 2017.
520 $a The rain shadow forests of the Olympic peninsula represent a unique, mixed-severity fire regime class in the midst of a highly productive landscape where spatial heterogeneity of fire severity may have significant implications for below and aboveground post-fire recovery. The purpose of this study was to quantify the impacts of wildfire on forest carbon (C) and nitrogen (N) pools and assess the influence of charcoal in a mixed-severity ecosystem on the Olympic Peninsula, Washington, USA. We established a fire chronosequence in forest stands ranging in time since fire (TSF) from 3 to 115 years prior to site establishment. At each site, we measured vegetation abundance, overstory composition, and attributes of surface mineral soil to a depth of 10 cm and forest floor organic matter that included pH, texture, bulk density, and C and N pools (dissolved organic C [DOC], phenol, ammonium, nitrate). Non-ionic resin lysimeters were buried at the interface of organic and mineral soil to measure the O-horizon leached DOC that would contact charcoal particles on the forest floor. Charcoal particles collected from the chronosequence sites were used in adsorption batch experimentation with phenol as a sorbate and measured an average 29.70 (+/- 6.23) mug phenol mg charcoal -1 adsorption capacity, which did not differ significantly between chronosequence sites. Wildfire-produced charcoal along the chronosequence showed high variability in adsorption capacity, which was partially explained by the thermogravimetric region of volatilized adsorbed compounds onto charcoal surfaces. The O-horizon leachate averaged 1.05 (SD +/- 2.87) g DOC m-2 year-1 and increased significantly along the TSF gradient (Pearson's r = 0.52; p < 0.0001). Multivariate, non-parametric analysis of soil and vegetation factors showed a significant relationship with the time since fire gradient between sites (p-value < 0.01) but not within sites. The TSF gradient was significantly correlated to charcoal mass in the O-horizon (r = -0.4), O-horizon C (r = 0.4), phenolic content in both O-horizon (r = 0.4) and mineral soils (r = 0.2), and potentially mineralizable N ( r = 0.4). Recent sites contained higher mineral soil total N and inorganic available N, though not significantly correlated with the TSF gradient. Over time, soils appear to shift toward phenolic-rich organic and mineral soils, higher moss cover, and a higher potentially mineralizable nitrogen index. This study provides evidence of a multivariate, belowground soil response that is less sensitive to wildfire disturbances than the aboveground vegetation.
590 $a School code: 0250.
650 4 $a Soil sciences. $3 2122699
650 4 $a Biogeochemistry. $3 545717
650 4 $a Environmental science. $3 677245
690 $a 0481
690 $a 0425
690 $a 0768
710 2 $a University of Washington. $b Environmental and Forest Science. $3 3278420
773 0 $t Dissertation Abstracts International $g 78-09B(E).
790 $a 0250
791 $a Ph.D.
792 $a 2017
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10257267