GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 2020-2022  (1)
  • 1990-1994  (1)
Document type
Publisher
Years
Year
  • 1
    ISSN: 1432-0703
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Medicine
    Notes: Abstract Principal-components analysis (PCA) was used to compare concentrations of polychlorinated dibenzo-p-dioxin (PCDD) and polychlorinated dibenzofuran (PCDF) compounds in sediments collected from two interconnected lakes, Lake Champlain and Lake George, New York, USA. Two different PCDD/PCDF congener profiles were present in surface sediment samples from Lake George. Samples collected near residential areas and power-boat marinas had elevated hepta- and octa-CDDs (1±0.3 ng/g) and tetra-octa-CDFs compared with samples collected in other areas of the lake. The PCDD/PCDF pattern in the high-level samples was similar to the PCDD/PCDF pattern in sediments from Green Lake, NY, a small lake in which atmospheric deposition is the only route for PCDD/PCDF contamination, either from local sources or from long range transportation from multiple sources in the midwest. The samples containing the higher PCDD/PCDF concentrations also contained higher lead concentrations (173±33 μg/g) compared to the low-level PCDD/PCDF samples (52±25 μg/g). However, the increase in lead concentrations was accompanied by increased concentrations of other trace metals. Consequently, it can be concluded that emissions from power boats are not responsible for the PCDD/PCDF contamination in Lake George. Concentrations of PCDDs/PCDFs in the low-level samples were similar to PCDD/PCDF concentrations in sediments from remote midwestern lakes where long range atmospheric deposition was the only plausible route of entry for the PCDD/PCDF compounds. However, other studies have shown that offshore sediments in Lake George have lower concentrations of organic carbon than inshore samples and, therefore, the low-level PCDD/PCDF pattern may be an artifact related to a reduced PCDD/PCDF concentration in sediments with a low organic carbon content. Surface and core sediments from Lake Champlain also partitioned into two groups, which both had PCDD/PCDF patterns differing from the high-level surface sediments collected from Lake George. The largest group of samples was characterized by the presence of high octa-CDD concentrations (3.5–18 ng/g). The second group of samples was four sections from a single core sample collected near a bleached kraft pulp and paper mill, which closed in 1970. These samples had high concentrations of tetra-CDFs (0.5–1.4 ng/g), primarily 2,3,7,8-tetra-CDF, accompanied by comparable concentrations of octa-CDD (0.9–4.4 ng/g). The presence of 2,3,7,8-tetra-CDF is consistent with results from several studies where PCDDs/PCDFs were analyzed in samples taken from various stages of the bleached kraft process. These samples were grouped in the same quadrant on a PCA plot as coal soot and pulp and paper mill sludge. However, the grouping was not close, and the PCDD/PCDF contamination in these sediments cannot be associated with either source. Five sections of a core collected near a currently operating bleached kraft pulp and paper mill also had elevated 2,3,7,8-tetra-CDF concentrations (0.3±0.05 ng/g), but these 2,3,7,8-tetra-CDF concentrations were accompanied by considerably higher octa-CDD concentrations (7.5±0.5 ng/g). Therefore, they could not be distinguished by PCA from the majority of the Lake Champlain samples.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2020-12-10
    Description: Back to top Wildfire occurrence is influenced by climate, vegetation and human activities. A key challenge for understanding the risk of fires is quantifying the mediating effect of vegetation on fire regimes. Here, we explore the relative importance of Holocene land cover, land use, dominant functional forest type, and climate dynamics on biomass burning in temperate and boreo-nemoral regions of central and eastern Europe over the past 12 kyr. We used an extensive data set of Holocene pollen and sedimentary charcoal records, in combination with climate simulations and statistical modelling. Biomass burning was highest during the early Holocene and lowest during the mid-Holocene in all three ecoregions (Atlantic, continental and boreo-nemoral) but was more spatially variable over the past 3–4 kyr. Although climate explained a significant variance in biomass burning during the early Holocene, tree cover was consistently the highest predictor of past biomass burning over the past 8 kyr. In temperate forests, biomass burning was high at ∼45 % tree cover and decreased to a minimum at between 60 % and 70 % tree cover. In needleleaf-dominated forests, biomass burning was highest at ∼ 60 %–65 % tree cover and steeply declined at 〉65 % tree cover. Biomass burning also increased when arable lands and grasslands reached ∼ 15 %–20 %, although this relationship was variable depending on land use practice via ignition sources, fuel type and quantities. Higher tree cover reduced the amount of solar radiation reaching the forest floor and could provide moister, more wind-protected microclimates underneath canopies, thereby decreasing fuel flammability. Tree cover at which biomass burning increased appears to be driven by warmer and drier summer conditions during the early Holocene and by increasing human influence on land cover during the late Holocene. We suggest that long-term fire hazard may be effectively reduced through land cover management, given that land cover has controlled fire regimes under the dynamic climates of the Holocene.
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...