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The National Mercury (Hg) Assessment in Norway evaluates the connections among: (a) national, regional and global Hg policies and regulations, (b) emissions, releases, uses and exposure pathways of Hg, and (c) concentrations of Hg in the environment, biota, and humans, measured during 2000-2020. Our findings suggest that the key changes of Hg in humans and the environment are highly dependent on the quality of the datasets, yet connections both to national and regional sources, as well as climate related drivers could be made for some data sets.
Norwegian Environment Agency
2022
2023
National report for Norway. WMO Global Ozone Research and Monitoring Project, report no. 48. WMO TD no. 1299
2005
2011
2006
2007
2008
2013
2023
2014
2005
2007
2008
Nedfall av tungmetaller rundt norske industrier studert ved analyse av mose: Undersøkelse i 2005. TA-2240/2007
2007
Nedfall av tungmetaller rundt norske industrier studert ved analyse av mose: Undersøkelse i 2010. NILU OR
Etter oppdrag fra Klima- og forurensningsdirektoratet er det gjennomført en undersøkelse av atmosfærisk nedfall av tungmetaller i nærområdet til 16 industribedrifter på 13 forskjellige steder i Norge. Undersøkelsen er basert på analyse av moseprøver innsamlet lokalt rundt hver enkelt bedrift sommeren 2010, og omfatter 59 elementer. I et flertall av tilfellene dreier det seg om gjentakelse av tilsvarende undersøkelser i 2000 og 2005.
2011
Nedfall av tungmetaller rundt utvalgte norske industrier. Studert ved analyse i mose. Statlig program for forurensningsovervåking. Rapport 831/2001. TA 1819/2001.
2001
2001
Negative correlation between soil salinity and soil organic carbon variability
Soil organic carbon (SOC) is vital for terrestrial ecosystems, affecting biogeochemical processes, and soil health. It is known that soil salinity impacts SOC content, yet the specific direction and magnitude of SOC variability in relation to soil salinity remain poorly understood. Analyzing 43,459 mineral soil samples (SOC < 150 g kg−1) collected across different land covers since 1992, we approximate a soil salinity increase from 1 to 5 dS m−1 in croplands would be associated with a decline in mineral soils SOC from 0.14 g kg−1 above the mean predicted SOC (= 18.47 g kg−1) to 0.46 g kg−1 below (~−430%), while for noncroplands, such decline is sharper, from 0.96 above = 35.96 g kg−1 to 4.99 below (~−620%). Although salinity’s significance in explaining SOC variability is minor (<6%), we estimate a one SD increase in salinity of topsoil samples (0 to 7 cm) correlates with respective declines of ~4.4% and ~9.26%, relative to and. The decline in croplands is greatest in vegetation/cropland mosaics while lands covered with evergreen needle-leaved trees are estimated with the highest decline in noncroplands. We identify soil nitrogen, land cover, and precipitation Seasonality Index as the most significant parameters in explaining the SOC’s variability. The findings provide insights into SOC dynamics under increased soil salinity, improving understanding of SOC stock responses to land degradation and climate warming.
2024