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Krysell, Mikael
Publikasjoner (4 av 4) Visa alla publikasjoner
Krysell, M. (1997). How accreditation changed us. Paper presented at EC QUASIMEME Final Workshop, MAR 13-17, 1996, CRIEFF, SCOTLAND. Marine Pollution Bulletin, 35(1-6), 167-168
Åpne denne publikasjonen i ny fane eller vindu >>How accreditation changed us
1997 (engelsk)Inngår i: Marine Pollution Bulletin, ISSN 0025-326X, E-ISSN 1879-3363, Vol. 35, nr 1-6, s. 167-168Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Today, laboratories involved in national or international marine monitoring programmes are strongly encouraged to seek accreditation or another formal proof of competence, The question often asked is whether a laboratory actually produces more reliable data when a quality system has been set up. A method of monitoring the differences in laboratory performance from year to year is presented in this paper. In the case of the SMHI Oceanographical Laboratory there has been substantial improvement in laboratory performance since formal quality assurance measures were introduced. (C) 1997 Elsevier Science Ltd. All rights reserved.

HSV kategori
Forskningsprogram
Oceanografi
Identifikatorer
urn:nbn:se:smhi:diva-1569 (URN)10.1016/S0025-326X(97)80881-8 (DOI)000072900800020 ()
Konferanse
EC QUASIMEME Final Workshop, MAR 13-17, 1996, CRIEFF, SCOTLAND
Tilgjengelig fra: 2015-09-02 Laget: 2015-08-31 Sist oppdatert: 2018-01-11bibliografisk kontrollert
Krysell, M., FOGELQVIST, E. & TANHUA, T. (1994). APPARENT REMOVAL OF THE TRANSIENT TRACER CARBON-TETRACHLORIDE FROM ANOXIC SEAWATER. Geophysical Research Letters, 21(23), 2511-2514
Åpne denne publikasjonen i ny fane eller vindu >>APPARENT REMOVAL OF THE TRANSIENT TRACER CARBON-TETRACHLORIDE FROM ANOXIC SEAWATER
1994 (engelsk)Inngår i: Geophysical Research Letters, ISSN 0094-8276, E-ISSN 1944-8007, Vol. 21, nr 23, s. 2511-2514Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Two chlorofluorocarbons (CFC-11 and carbon tetrachloride, CCl4) widely used as tracers for dating water masses, were measured in the Gotland Basin of the Baltic Sea. At the time of the survey, the bottom water of the basin had remained stagnant for 15 years and anoxic for about the same period of time, and the concentrations of both CFC-11 and CCl4 decrease dramatically with depth below the mixed layer. Furthermore, the ratio of CFC-11 to CCl4 increases with depth under the mixed layer along with a steep decrease in oxygen concentration. This is contrary to what would be expected from the atmospheric histories. The most plausible explanation for this is that there is a mechanism whereby the CCl4 is removed from the water mass under anoxic and suboxic conditions.

sted, utgiver, år, opplag, sider
GOTHENBURG UNIV,DEPT ANALYT & MARINE CHEM,S-41296 GOTHENBURG,SWEDEN. SMHI,OCEANOG LAB,GOTHENBURG,SWEDEN.: , 1994
HSV kategori
Forskningsprogram
Oceanografi
Identifikatorer
urn:nbn:se:smhi:diva-1659 (URN)10.1029/94GL02336 (DOI)A1994PT47400016 ()
Tilgjengelig fra: 2016-01-26 Laget: 2015-12-22 Sist oppdatert: 2018-01-10bibliografisk kontrollert
Andersson, L., Sjöberg, B. & Krysell, M. (1994). The conditions of the seas around Sweden: Report from the activities in 1993. SMHI
Åpne denne publikasjonen i ny fane eller vindu >>The conditions of the seas around Sweden: Report from the activities in 1993
1994 (engelsk)Rapport (Annet vitenskapelig)
sted, utgiver, år, opplag, sider
SMHI, 1994
Serie
RO, Rapport Oceanografi, ISSN 0283-1112 ; 20
Emneord
koncentration, vatten, atmosfären
Identifikatorer
urn:nbn:se:smhi:diva-2658 (URN)Oceanografi, Rapporter, Serie RO (Lokal ID)Oceanografi, Rapporter, Serie RO (Arkivnummer)Oceanografi, Rapporter, Serie RO (OAI)
Tilgjengelig fra: 1994-09-17 Laget: 2016-07-08 Sist oppdatert: 2016-07-08bibliografisk kontrollert
Fogelqvist, E. & Krysell, M. (1991). NATURALLY AND ANTHROPOGENICALLY PRODUCED BROMOFORM IN THE KATTEGATT, A SEMIENCLOSED OCEANIC BASIN. Journal of Atmospheric Chemistry, 13(4), 315-324
Åpne denne publikasjonen i ny fane eller vindu >>NATURALLY AND ANTHROPOGENICALLY PRODUCED BROMOFORM IN THE KATTEGATT, A SEMIENCLOSED OCEANIC BASIN
1991 (engelsk)Inngår i: Journal of Atmospheric Chemistry, ISSN 0167-7764, E-ISSN 1573-0662, Vol. 13, nr 4, s. 315-324Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

The origin of bromoform in seawater and atmosphere, as well as possible sinks and breakdown mechanisms, is discussed. A bromoform budget is calculated for the Kattegatt area between Sweden and Denmark, where the input of bromoform from a power plant is significant. Both anthropogenically (250 x 10(6) g yr-1) and biogenically (350 x 10(6) g yr-1, 0.016 g m-2 yr-1) produced bromoform is likely to have a great impact locally on the inventory and the release to the atmosphere. Using measured sur-face concentrations of bromoform, the total annual release from the Kattegatt to the atmosphere is estimated to 550 x 10(6) g (0.025 g m-2 yr-1).

sted, utgiver, år, opplag, sider
CHALMERS UNIV TECHNOL,DEPT ANALYT & MARINE CHEM,S-41296 GOTHENBURG,SWEDEN. GOTHENBURG UNIV,S-41296 GOTHENBURG,SWEDEN.: , 1991
Emneord
BROMOFORM, BIOGENIC BROMOFORM, ANTHROPOGENIC BROMOFORM, SEAWATER CHLORINATION, AIR-SEA EXCHANGE, KATTEGATT
HSV kategori
Forskningsprogram
Oceanografi
Identifikatorer
urn:nbn:se:smhi:diva-1708 (URN)10.1007/BF00057749 (DOI)A1991HK29700001 ()
Tilgjengelig fra: 2016-02-03 Laget: 2016-02-02 Sist oppdatert: 2018-01-10bibliografisk kontrollert
Organisasjoner
v. 2.35.7
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