2011
DOI: 10.1029/2011wr010977
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Controls on stream water dissolved mercury in three mid‐Appalachian forested headwater catchments

Abstract: [1] Determining the controls on dissolved mercury (Hg D ) transport is necessary to improve estimations of export from unmonitored watersheds and to forecast responses to changes in deposition and other environmental forcings. Stream water Hg D and dissolved organic carbon (DOC) were evaluated over a range of discharge conditions in three streams within Shenandoah National Park, VA. Watersheds are distinguished by stream water pH (ranging from neutral to acidic) and soil size fractioning (ranging from clays to… Show more

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Cited by 38 publications
(50 citation statements)
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References 100 publications
(143 reference statements)
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“…3-17B). These findings are consistent with our understanding that organic carbon binds strongly with total and methylmercury (Grigal, 2002;Hall and others, 2008;Riscassi and Scanlon, 2011).…”
Section: Mercury In Streams Is Controlled By Dissolved Organic Carbonsupporting
confidence: 81%
“…3-17B). These findings are consistent with our understanding that organic carbon binds strongly with total and methylmercury (Grigal, 2002;Hall and others, 2008;Riscassi and Scanlon, 2011).…”
Section: Mercury In Streams Is Controlled By Dissolved Organic Carbonsupporting
confidence: 81%
“…On the other hand, Stoken et al () found no relationship between ratio of Hg D :DOC and atmospheric wet Hg deposition across the US. These authors conclude that the amount of Hg freshly deposited is not the dominant factor explaining the spatial variability in the coupling between Hg and DOC and subsequent transport in the system (Riscassi & Scanlon, ; Stoken et al, ). In addition, the recent deposition may not accurately reflect the historical Hg accretion in soil due to a time lag between the two sources, which could explain the negative (or lack of) relationship between Hg:DOC and fresh Hg input (Stoken et al, ).…”
Section: Discussionmentioning
confidence: 99%
“…For the difference between Hg–DOC and Hg–Aromatic portion of DOC (UV 254 , SUVA 254 , UV 420 , and UV 320 ) in objective 3, we ran a multivariate model with DOC type as random (repeated) variable nested within the Study using the function rma.mv in the metafor package (Viechtbauer, ). We used studies that measured both DOC and a measure of aromaticity, which led to 10 studies with 16 pairwise comparisons for THg (Bravo et al, ; Burns et al, ; Dittman et al, ; Eklöf et al, ; Eklöf et al, ; Jeremiason et al, ; MacMillan et al, ; Navratil et al, ; Riscassi et al, ; Riscassi & Scanlon, ) and 4 studies with 6 pairwise comparisons for MeHg (Bravo et al, ; Eklöf et al, ; Jeremiason et al, ; MacMillan et al, ). The most widespread measure of aromaticity was SUVA 254 , which is the specific UV absorbance at 254 nm divided by DOC concentration (UV 254 /DOC).…”
Section: Methodsmentioning
confidence: 99%
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“…Fishing Brook was sampled at the outlet of County Line Flow, a small shallow impoundment just upstream of the USGS stream gage that recorded stage at 15-min intervals for conversion to streamflow through a rating curve (Rantz et al 1982). All stream samples were collected by wading to the center point of flow or reaching to the center of flow when channels were narrow or to sample groundwater seeps.…”
Section: Field Samplingmentioning
confidence: 99%