أعرض تسجيلة المادة بشكل مبسط
dc.contributor |
Schoenholtz, Stephen H. |
|
dc.contributor |
Powers, Robert F. |
|
dc.contributor |
Perakis, Steven S. |
|
dc.contributor |
Myrold, David D. |
|
dc.contributor |
Murphy, Glen E. |
|
dc.contributor |
Hansen, Eric N. |
|
dc.date |
2007-08-15T15:11:43Z |
|
dc.date |
2007-08-15T15:11:43Z |
|
dc.date |
2007-07-27 |
|
dc.date |
2007-08-15T15:11:43Z |
|
dc.date.accessioned |
2013-10-16T08:08:22Z |
|
dc.date.available |
2013-10-16T08:08:22Z |
|
dc.date.issued |
2013-10-16 |
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dc.identifier |
http://hdl.handle.net/1957/6343 |
|
dc.identifier.uri |
http://koha.mediu.edu.my:8181/xmlui/handle/1957/6343 |
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dc.description |
Graduation date: 2008 |
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dc.description |
Belowground carbon (C) storage and quality of soil organic matter (SOM) in
forest soils have implications for sustainable forest management and C sequestration,
but how these pools change in response to management is poorly understood. I
investigated whether fertilization and competing vegetation control, applied alone or
in combination early in stand development, affected forest-floor, fine-root, and
mineral-soil C and nitrogen (N) pools to 1-m depth at three ponderosa pine (Pinus
ponderosa) plantations across a site-quality gradient in northern California. Secondly,
I assessed how these treatments affected surface SOM quality at these sites via 1)
density fractionation, 2) dissolved organic C (DOC) and dissolved N release during
225-day laboratory incubation, and 3) CO2 evolution and DOC mobilization during
16-day laboratory incubation.
Twenty years after plantation establishment, mean belowground C pools, were 83,
177, and 206 Mg C ha-1 for the low-, intermediate-, and high-quality sites,
respectively. Belowground N pools for the three sites were 5.6, 7.4, and 6.8 Mg N
ha-1, respectively. Responses of aboveground biomass to treatment were marked, but
changes in belowground C and N pools to fertilization and competing vegetation
control were limited. Fertilization increased total C and N pools at the low- and
intermediate-quality sites and increased the proportion of total belowground C and N
in the forest floor at all three sites. Competing vegetation control increased the forestfloor
C pool at the lowest quality site, but had no effect on total pools. Fertilizer
increased whole-soil and light-density-fraction N and decreased C:N ratios at two
sites, suggesting increased SOM quality. Fertilization decreased C mineralization at
the most productive site, had the opposite effect at the intermediate site, and had no
effect at the poor site. Competing vegetation control affected light-fraction C and N
concentrations and C:N ratios inconsistently among sites and decreased N
mineralization at the most productive site, suggesting decreased SOM quality.
Although forest floors were the most sensitive of the belowground C pools to these
silvicultural treatments, results suggest that the major mechanism for increased C
sequestration through management of these ponderosa pine forests will be through
increased tree growth, rather than belowground C storage. |
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dc.language |
en_US |
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dc.subject |
forest soils |
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dc.subject |
forest management |
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dc.subject |
carbon quality |
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dc.subject |
carbon sequestration |
|
dc.title |
Belowground carbon storage and soil organic matter quality following fertilizer and
herbicide applications in ponderosa pine plantations along a site-quality gradient in
northern California |
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dc.type |
Thesis |
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أعرض تسجيلة المادة بشكل مبسط