0000000000053023

AUTHOR

Markus Hannula

showing 3 related works from this author

How and why does willow biochar increase a clay soil water retention capacity?

2018

Addition of biochar into a soil changes its water retention properties by modifying soil textural and structural properties. In addition, internal micrometer-scale porosity that is able to directly store readily plant available water affects soil water retention properties. This study shows how precise knowledge of the internal micrometer-scale pore size distribution of biochar can deepen the understanding of the biochar-water interactions in soils. The micrometer-scale porosity of willow biochar was quantitatively and qualitatively characterized using X-ray tomography, 3D image analysis and Helium ion microscopy. The effect of biochar application on clay soil water retention was studied by…

Water retention curveSoil science010501 environmental sciencesmikroskopia01 natural sciencessavihuokoisuussoil water retentiontomografiaBiocharSurface roughnessmedicine3D image analysisbiochar3D-mallinnusPorosityta216Waste Management and DisposalWater contentta2180105 earth and related environmental sciences219 Environmental biotechnologybiohiilimaaperäta114Renewable Energy Sustainability and the EnvironmentChemistryForestry04 agricultural and veterinary sciences15. Life on land6. Clean waterWater retentionmikrorakenteetSoil structureplant available waterSoil water040103 agronomy & agriculturehelium ion microscopy0401 agriculture forestry and fisheriesmedicine.symptomvesipitoisuusAgronomy and Crop ScienceX-ray tomographyBiomass and Bioenergy
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Effects of pyrolysis temperature on the hydrologically relevant porosity of willow biochar

2018

Biochar pore space consists of porosity of multiple length scales. In direct water holding applications like water storage for plant water uptake, the main interest is in micrometre-range porosity since these pores are able to store water that is easily available for plants. Gas adsorption measurements which are commonly used to characterize the physical pore structure of biochars are not able to quantify this pore-size range. While pyrogenetic porosity (i.e. pores formed during pyrolysis process) tends to increase with elevated process temperature, it is uncertain whether this change affects the pore space capable to store plant available water. In this study, we characterized biochar poro…

porosityMaterials scienceFOS: Physical sciencesApplied Physics (physics.app-ph)010501 environmental sciencesRaw materialkuivatislaus01 natural sciencesAnalytical ChemistryhuokoisuusAdsorptionimage analysisBiocharmedicinebiocharta216CharcoalPorosityta2180105 earth and related environmental sciencesCondensed Matter - Materials Sciencex-ray tomographybiohiilita114Materials Science (cond-mat.mtrl-sci)Physics - Applied Physics04 agricultural and veterinary sciencesAtmospheric temperature rangeslow pyrolysisWater retentionFuel TechnologykuvantaminenChemical engineeringvisual_artkuva-analyysi040103 agronomy & agriculturevisual_art.visual_art_medium0401 agriculture forestry and fisheriesmedicine.symptomPyrolysis
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Aritmeettis-geometris-harmoninen keskiarvoepäyhtälö

2008

matematiikkakeskiarvotaritmetiikkageometriaepäyhtälöt
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