Publikasjoner
NIBIOs ansatte publiserer flere hundre vitenskapelige artikler og forskningsrapporter hvert år. Her finner du referanser og lenker til publikasjoner og andre forsknings- og formidlingsaktiviteter. Samlingen oppdateres løpende med både nytt og historisk materiale. For mer informasjon om NIBIOs publikasjoner, besøk NIBIOs bibliotek.
2002
Forfattere
Toril Drabløs EldhusetSammendrag
Det er ikke registrert sammendrag
Sammendrag
Det er ikke registrert sammendrag
Forfattere
Tor MykingSammendrag
Det er ikke registrert sammendrag
Sammendrag
Det er ikke registrert sammendrag
Forfattere
Terje Birkeland P.J. Houen Erlend Ystrøm Haartveit V. Kilde P. Lind Knut Magnar Sandland Kjell Vadla Audun ØvrumSammendrag
Det er ikke registrert sammendrag
Forfattere
Nicholas ClarkeSammendrag
In natural waters, total organic carbon (TOC) is the sum of particulate and dissolved organic carbon. Dissolved organic carbon (DOC) is operationally defined, usually as organic carbon that passes through a 0.45 µm filter. Cellulose acetate or nitrate filters should not be used for this purpose due to contamination or adsorption problems. Glass fibre filters are preferable. Although the discussion below concerns DOC, much of it applies to TOC as well. Organic carbon is most often determined after oxidation to CO2 using combustion, an oxidant such as persulphate, UV or other high-energy radiation, or a combination of some of these. If only UV radiation with oxygen as oxidant is used, low DOC values may be obtained in the presence of humic substances. A variety of methods are used for detection, including infrared spectrometry, titration and flame ionization detection after reduction to methane. Always follow the instrument manufacturer’s instructions. For determination of dissolved organic carbon, dissolved inorganic carbon must be either removed by purging the acidified (for example with phosphoric acid) sample with a gas which is free from CO2 and organic compounds, or determined and subtracted from the total dissolved carbon. If acidification followed by purging is used, care should be taken as volatile organic compounds may also be lost. After acidification, remove CO2 by blowing a stream of pure carbon-free inert gas through the system for at least 5 minutes. Carbon is ubiquitous in nature, so reagents, water, and glassware cannot be completely cleaned of it. Method interferences (positive bias) may be caused by contaminants in the carrier gas, dilution water, reagents, glassware, or other sample processing hardware (for example a homogenization device). All of these materials must be routinely demonstrated to be free from interference under the conditions of analysis by running reagent blanks. Plastic bottles can bleed carbon into water samples, especially when they are new, or when they are used for low-level samples (less than 200 ppb C). Any new bottles (especially plastic) should ideally be filled with clean water for a period of several days or boiled in water for a few hours before use. The use of high purity or purified reagents and gases helps to minimise interference problems. It is very important to use ultra-pure water with a carbon filter or boiled distilled water just before preparing stock and standard solutions, in order to remove dissolved CO2. The stock solution should not be kept too long (about one week). For most DOC instruments a correction for DOC (due to dissolved CO2) in the dilution water used for calibration standards is necessary, especially for standards below 10 ppm C. The carbon in the blank should only be subtracted from standards and not from samples. For calibration, standard solutions are most often potassium hydrogen phthalate for total dissolved carbon and sodium bicarbonate for dissolved inorganic carbon. The DOC concentration should be within the working range of the calibration. If necessary the sample can be diluted. Sample DOC below about 50 ppb C can be affected by atmospheric exposure. In these cases, sampling bottles should be kept closed when possible, and autosampler vials should be equipped with septa for needle piercing by the autosampler.
Forfattere
Peder GjerdrumSammendrag
This dissertation addresses questions of timber quality in the interface between the forestry and the sawmill. The labour was carried out in an industrial environment for the benefit of the sawmill industry and - in a wider scope - for the entire wood chain. Specimens from a total of more than three thousand five hundred softwood sawlogs and trees were investigated for heartwood, spiral grain or log geometry. Applying analytic and statistical tools, several models for wood properties were built. For pine heartwood the samples spanned most growth conditions and forested areas in the Scandinavian Peninsula. Age was found to be the predominant factor in heartwood formation. A global model termed the Heartwood Age Law could be recognised: Heartwood age, at arbitrary height in the tree, equals the square root of cambial age less three, to the second power. This finding might be used for heartwood modelling. Based on temperature gradients between the sap- and heartwood, an algorithm for calculating the heartwood diameter fraction in an IR image was established. Used in conjunction with a scanner, the following model was established: Top end heartwood diameter might be calculated by multiplying top end diameter observed in a shadow scanner with heartwood diameter fraction estimated from an IR image of arbitrary end of the log. The observed temperature gradient between heart- and sapwood indicated the accuracy of the method. In the industry, IR heartwood detection might be applied in sorting sawlogs to produce timber of distinct properties. Further, correlation to properties like ring width and knots, and to time since harvest, was suggested. A constant change rate in grain angle was found for the mature part of spruce sawlogs. Albeit great variability in intercept and inclination, a linear pattern in grain angle to radial distance from the pith prevailed for specimens from both of the two separated Nordic samples. A combined model including the juvenile zone around the pith was suggested. Two parameters are sufficient to model the grain angle for the entire radial range from the pith to the mantle in any spruce specimen. The main impact of the finding might be for use in modelling and simulation. Derived from observations in a 3D scanner, four parameters describing the centroid of sawlogs were calculated. Based on these parameters several distinct crook types could be classified in an automated routine: First, straight logs were separated from crooked ones; then smooth and simple sweep (that might be accepted in sawlogs) were separated from abrupt crook. Even more specific crook classes could be identified. In an industrial application, this model might increase the speed and reliability of sawlog classification. Observing the log diameter on or under bark and the cross-sectional shape of a sawlog both have an impact on the yield. Optimal yield was only obtained after accurate observing the diameter under bark, integrated in the conversion process. Based on actually observed crosscut shapes, simulation indicated that this strategy might produce up to one tenth more main yield as compared to diameter observation in one direction before barking. Other methods were intermediate. Further investigations analysing the variation in crosscut shape along the stem and the accuracy of observation were recommended.
Forfattere
Peder Gjerdrum I. AkerfeldsSammendrag
Det er ikke registrert sammendrag
Sammendrag
Det er ikke registrert sammendrag
Forfattere
A. Sæbø Vegard Gundersen S. Nyhuus P.A. PedersenSammendrag
Det er stort behov for utvikling av gode grøntanlegg til lek, trim og rekreasjon der folk bor. Imidlertid blir det satset alt for lite på en nyutvikling på dette området. Det er behov for forskning og utvikling innenfor planlegging, plantevalg, etablering og skjøtsel. Resultatene vil kunne bidra til høyere kvalitet og at vi får mer igjen for kronene som investeres.