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dc.contributor.authorErisman JW
dc.date.accessioned2012-12-12T22:40:29Z
dc.date.available2012-12-12T22:40:29Z
dc.date.issued1991-01-31
dc.identifier723001002
dc.identifier.urihttp://hdl.handle.net/10029/261661
dc.description.abstractAbstract niet beschikbaar
dc.description.abstractIn this report dry and wet deposition of acid components and acidifying substances in the Netherlands are presented. The depositions were estimated from measurements of concentrations in the atmosphere and in precipitation. The method has been applied for the Netherlands on a 5 x 5 km2 scale. The emphasis has been on estimating the deposition fluxes to nature areas in the Netherlands. In 1989 the total potential acid deposition was estimated to be 4800 mol H+/ha-1/a-1 (28% SOx, 24% NOy, 46% NHx and 2% HCl). In 1980 the potential acid deposition was estimated to be 6800 mol H+/ha-1/a-1. The decrease in 1989 with respect to 1980 is mainly the result of the lower SOx deposition. Dry deposition on forests in the Netherlands is on the average 20% higher for SOx, NOy and NHx. Dry deposition on heathland was estimated 10% higher for SOx, NOy and NHx. Dry deposition on moorland pools was estimated 120% higher for SOx, 40% lower for NOy and 90% higher for NHx than for the average Dutch landscape. The estimated uncertainty in the potential acid deposition flux is about range 44-80% for 5 x 5 km2 grids and 16-48% for the Netherlands on the whole.
dc.description.sponsorshipDGM/L
dc.format.extent81 p
dc.language.isoen
dc.relation.ispartofRIVM Rapport 723001002
dc.relation.urlhttp://www.rivm.nl/bibliotheek/rapporten/723001002.html
dc.subject15nl
dc.subject91-1nl
dc.subjectdepositionnl
dc.subjectacidifying componentsnl
dc.subjectnature areasnl
dc.titleAcid deposition in the Netherlandsen
dc.title.alternativeZure depositie in Nederlandnl
dc.typeReport
dc.date.updated2012-12-12T22:40:30Z
html.description.abstractAbstract niet beschikbaar
html.description.abstractIn this report dry and wet deposition of acid components and acidifying substances in the Netherlands are presented. The depositions were estimated from measurements of concentrations in the atmosphere and in precipitation. The method has been applied for the Netherlands on a 5 x 5 km2 scale. The emphasis has been on estimating the deposition fluxes to nature areas in the Netherlands. In 1989 the total potential acid deposition was estimated to be 4800 mol H+/ha-1/a-1 (28% SOx, 24% NOy, 46% NHx and 2% HCl). In 1980 the potential acid deposition was estimated to be 6800 mol H+/ha-1/a-1. The decrease in 1989 with respect to 1980 is mainly the result of the lower SOx deposition. Dry deposition on forests in the Netherlands is on the average 20% higher for SOx, NOy and NHx. Dry deposition on heathland was estimated 10% higher for SOx, NOy and NHx. Dry deposition on moorland pools was estimated 120% higher for SOx, 40% lower for NOy and 90% higher for NHx than for the average Dutch landscape. The estimated uncertainty in the potential acid deposition flux is about range 44-80% for 5 x 5 km2 grids and 16-48% for the Netherlands on the whole.


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