{"title":"Glensaugh - United Kingdom","id":{"prefix":"https:\/\/deims.org\/","suffix":"1c4d454d-0c00-49f9-a7fe-3a3e596c3648"},"type":"site","created":"2012-12-25T19:02:12+01:00","changed":"2023-07-28T10:01:12+02:00","attributes":{"affiliation":{"networks":[{"network":{"name":"COSMOS-UK","id":{"prefix":"https:\/\/deims.org\/networks\/","suffix":"d97bd527-9101-4df1-afb5-cfe9ce9aa489"}},"siteCode":null,"verified":false},{"network":{"name":"ILTER","id":{"prefix":"https:\/\/deims.org\/networks\/","suffix":"1aa7ccb2-a14b-43d6-90ac-5e0a6bc1d65b"}},"siteCode":null,"verified":true},{"network":{"name":"LTER Europe","id":{"prefix":"https:\/\/deims.org\/networks\/","suffix":"4742ffca-65ac-4aae-815f-83738500a1fc"}},"siteCode":null,"verified":true},{"network":{"name":"UK ECN","id":{"prefix":"https:\/\/deims.org\/networks\/","suffix":"a197664f-569e-4df6-933a-86de676dbfc5"}},"siteCode":"LTER_EU_UK_048","verified":true},{"network":{"name":"UK Eutrophying and Acidifying atmospheric Pollutants network (UKEAP)","id":{"prefix":"https:\/\/deims.org\/networks\/","suffix":"47ccb7a9-ba65-4dd9-a564-4623d016d0ec"}},"siteCode":null,"verified":false}],"projects":[{"label":"eLTER (H2020)","uri":"https:\/\/cordis.europa.eu\/project\/id\/654359"},{"label":"eLTER PLUS (H2020) - VA","uri":"https:\/\/doi.org\/10.3030\/871128"}]},"contact":{"siteManager":[{"type":"person","name":"Helen Watson","email":"helen.watson@hutton.ac.uk","orcid":null}],"operatingOrganisation":[{"type":"organisation","name":"James Hutton Institute","url":"https:\/\/www.hutton.ac.uk\/","ror":"https:\/\/ror.org\/03rzp5127"}],"metadataProvider":[{"type":"person","name":"Andrew Sier [Primary ECN contact]","email":"arjs@ceh.ac.uk","orcid":null},{"type":"person","name":"David Hamilton [INACTIVE]","email":"david.hamilton@hutton.ac.uk","orcid":null}],"fundingAgency":null,"siteUrl":[{"title":"ECN website","value":"https:\/\/ecn.ac.uk\/"}]},"general":{"abstract":"UK ECN site. Glensaugh is one of two terrestrial ECN sites currently managed by the James Hutton Institute. \r\n\r\nGlensaugh Research station is 35 miles south west of Aberdeen, NE Scotland (NGR NO 671783), on the edge of the Grampian hills and covers over 1100 hectares. The dominant cover is semi-natural vegetation, and there is a small amount of woodland (5ha) and some short term and permanent grassland (150ha). Much of the ECN monitoring is carried out towards the northern boundary of the research station in the small upland catchment of the Birnie Burn. Winters can be severe and snow may lie in patches until late March.\r\n\r\nThe target sampling site is located at an altitude of 300m on heather dominated (Calluna vulgaris) moorland interspersed with patches of blaeberry (Vaccinium myrtillus). It has a westerly aspect and straight slopes of up to 20 degrees. The soil is predominantly freely draining humus iron podzol of the Strichen Series. The water chemistry sampling point, flume and in-stream measurements are made on the Birnie Burn at an altitude of 240m. The catchment area above the sampling point is around 100ha. Precipitation and atmospheric chemistry samples are collected adjacent to the stream at a similar altitude.","citation":null,"relatedIdentifiers":null,"status":{"label":"Operational","uri":"http:\/\/vocabs.lter-europe.net\/elter_cl\/10772"},"yearEstablished":1992,"yearClosed":null,"relatedSites":[{"typeOfRelationship":{"label":"contains","uri":"null"},"listOfSites":[{"type":"site","title":"Birnie Burn - United Kingdom","id":{"prefix":"https:\/\/deims.org\/","suffix":"8747ccf7-52af-4a83-a558-71a768b81a30"},"changed":"2023-07-28T09:55:48+0200"}]}],"siteName":"Glensaugh","shortName":"T02","siteType":"Stationary land-based site","protectionLevel":null,"landUse":null,"images":[{"url":"https:\/\/deims.org\/sites\/default\/files\/photos\/Glensaugh%2520Weather%2520Station%2520looking%2520toThorter%2520Hill.JPG","alt":"Automatic Weather Station at ECN Glensaugh"},{"url":"https:\/\/deims.org\/sites\/default\/files\/photos\/GS_Birnie.JPG","alt":"Monitoring equipment on the Birnie Burn, ECN Glensaugh"},{"url":"https:\/\/deims.org\/sites\/default\/files\/photos\/Cairn%2520Burn%2520Flume.JPG","alt":"Flume on Cairn Burn, ECN Glensaugh"},{"url":"https:\/\/deims.org\/sites\/default\/files\/photos\/GS_AWS_Winter.JPG","alt":"Automatic Weather Station at ECN Glensaugh, in the snow"}]},"environmentalCharacteristics":{"airTemperature":{"yearlyAverage":7.5,"monthlyAverage":null,"unit":"\u00b0C","referencePeriod":null},"precipitation":{"yearlyAverage":1128,"monthlyAverage":null,"unit":"mm","referencePeriod":null},"biogeographicalRegion":"atlantic","biome":"grasslands","ecosystemType":[{"label":"Agricultural","uri":null},{"label":"Fresh Water Rivers","uri":null},{"label":"Grasslands","uri":null},{"label":"Lakes","uri":null},{"label":"Rivers","uri":null},{"label":"Small lakes","uri":null},{"label":"Small rivers","uri":null},{"label":"Temperate grasslands, savannas, and shrublands","uri":null}],"eunisHabitat":[{"label":"Grasslands and lands dominated by forbs, mosses or lichens (E)","uri":null}],"landforms":null,"geoBonBiome":["Fresh water rivers","Terrestrial"],"geology":"The Highland Boundary Fault divides the Research Station into two distinct geological zones. North of the fault are drifts derived from schistose rock.  To the south of the fault are drifts derived from Old Red Sandstone. ","hydrology":"The area is drained by a number of  small headwater streams.  The ground water table is relatively high and there are many springs across higher ground. There is also a small loch. Some streams are virtually  emphemeral and run through deep gravels in the summer.","soils":"The soils reflect the underlying geology which is influenced by The Highland Boundary Fault. North of the fault the soils are of the Strichen Association.  Brown forest soils and podzols of the lower slopes give way to peaty podzols and, on the highest ground, to peat. To the south of the fault the soils are humus-iron podzols on the lower slopes and peaty podzols  at higher elevations.","vegetation":"The research station comprises 865 hectares (ha) of semi-natural plant communities, 60 ha of predominantly rotational grassland and 88 ha of permanent pasture. On the alluvial soils of the valley bottom the semi-natural vegetation is dominated by species-rich Agrostis-Festuca grassland. This gives way to species-poor Agrostis-Festuca on the lower slopes, with bracken (Pteridium aquilinum) also present. The higher slopes are dry heather (Calluna vulgaris) moor, with blaeberry (Vaccinium myrtillus), wavy hair grass (Deschampsia flexuosa) and bell heather (Erica cinerea) locally important. On the deeper peats at the highest altitude, cross-leaved heather (Erica tetralix) and cotton sedge (Eriophorum vaginatum) become co-dominant. The predominantly rotational grassland is reseeded with perennial ryegrass and white clover mixtures every 7-10 years. This provides grazing for the crossbred ewe flock, swards for experimental work, silage for winter feeding and aftermath grazing for finishing lambs."},"geographic":{"boundaries":"POLYGON ((-2.5389410646386 56.924885498862, -2.5382111479924 56.924751641826, -2.5373179066591 56.924791418277, -2.5363837213414 56.924911655593, -2.5353248042785 56.924998169737, -2.5332278037144 56.925228914634, -2.5323563831502 56.925360083701, -2.5314024546325 56.925538200159, -2.5305507425964 56.925612001937, -2.5298259146145 56.925799802116, -2.5289334290583 56.925931597991, -2.5284579200675 56.926106544215, -2.52787770771 56.926247680453, -2.5268606118565 56.926391217073, -2.526009385453 56.926464985791, -2.5256346549126 56.926432872885, -2.5258000195988 56.926363115677, -2.5258998370684 56.926086448119, -2.5260838157363 56.925843676628, -2.5262661782082 56.925486369878, -2.5265319961901 56.925185982319, -2.5268416855494 56.925011742181, -2.5272133231981 56.924825449007, -2.5277084105837 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