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wise use of mires and peatlands - Peatland Ecology Research Group

wise use of mires and peatlands - Peatland Ecology Research Group

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GLOSSARY OF CONCEPTS AND TERMS171Non-material lifesupport valuesNoocentrismN orgNormal problemsNormativeprinciplesNormsOligotrophicOmbrogenousOmbrotrophicOption functionOrganicOrganismicOrgano-mineralfertilisersOscillationOsmosisOxicOxidationOxidative peatlossesOzoneA range <strong>of</strong> values relating to the mind, sensation, <strong>and</strong> the spirit.Moral position that ascribes intrinsic value only to rational beings.Nitrogen in organic form.Problems that can be solved by progress <strong>and</strong>/or through investment.Principles <strong>of</strong> behaviour which make it possible to resolve valueconflicts in a rational way.Generalised expectations <strong>of</strong> behaviour, as in guidelines,conventions <strong>and</strong> laws.Poor to extremely poor in nutrients.Only receiving precipitation water.Only supplied with nutrients by the atmosphere.The same as bequest functions - those relating to what is leftfor future generations. Relate to the importance people place ona safe future.Material which results from carbon chemical biosynthesis.Relating to an organism as a whole.Combined organic <strong>and</strong> mineral fertilisers.Fluctuation; variation; change back <strong>and</strong> forth.The passage <strong>of</strong> water through a semi-permeable membrane into amore concentrated solution, ending by equalising theconcentrations on both sides <strong>of</strong> the membrane.Containing oxygen, aerobic. Usually <strong>use</strong>d in reference to amicrobial habitat.A reaction in which the atoms in an element lose electrons(<strong>of</strong>ten – but not limited to – to oxygen) See under ‘oxidativepeat losses’.Losses <strong>of</strong> peat resulting from the reaction <strong>of</strong> peat with oxygen(after drainage).An unstable gas in which three atoms <strong>of</strong> oxygen occur together.Ozone is a greenho<strong>use</strong> gas. In the atmosphere ozone occurs attwo different altitudes. Low altitude tropospheric ozone is a form<strong>of</strong> air pollution (part <strong>of</strong> smog) produced by the emissions fromcars <strong>and</strong> trucks. High in the atmosphere a thin layer <strong>of</strong>stratospheric ozone is naturally created by sunlight. This ozonelayer shields the earth from dangerous (cancer-causing)ultraviolet radiation from the sun. Several gases (notablychlor<strong>of</strong>luorocarbons, CFCs) speed the breakdown <strong>of</strong> ozone inthe ozone layer. While serious in its own right, this is largely adifferent problem from the problem <strong>of</strong> global warming. Abbreviatedas O 3.

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