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Ecological units and core locations for organic carbon and nutrient quantification

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Investigating permafrost coastal erosion and the resulting nutrient input in the western Canadian Arctic

Jaroslav Obu, Hugues Lantuit, Michael Fritz, Birgit Heim, Lutz Schirrmeister

Alfred Wegener Institute for Polar and Marine Research Potsdam

jaroslav.obu@awi.de

Project flow chart

Ecological units and core locations for organic carbon and nutrient quantification

Permafrost Coring

Study area

LIDAR Digital elevation model

One meter resolution DEM was obtained from LIDAR scanning of Yukon Coast and Herschel Island in

2012. DEM from year 2013 will be used to reveal chan- ges in landscape. Empha- sises will be on coastal erosion and different means of material trans- portation to sea.

• A pit was dug in active layer and permafrost was drilled with SIPRE corer up to 2 meters

• Cores were sampled for 5 cm samples each 10 cm

• They are being analysed for soil organic carbon and total nitrogen

Ecological classificati- on was produced from RapidEye multispect- ral satellite imagery and slope layer with maximal-likehood su- pervised classification.

Training areas for 8 predefined ecological units were delineated during the expedition to Herschel Island in 2013. 13 cores were drilled, at least one in each unit, to produce soil organic carbon and nutrient content map.

Study area of PhD project is Yukon Coast with Herschel Island. Both consist of unconso- lidated sediments, massive ice and are thus very exposed to coastal erosion. Herschel Island is ice-thrusted moraine and terrain is moderately sloping with mostly steep coastal bluffs. Yukon Coastal Plain is flat and gently sloping with steep coasts, retrogressive

thaw slumps, spits and barrier islands. Area has polar tundra climate with harsh winters and summer mean temperatures above 0°C.

Rapid environmental changes in the Arctic, including permafrost thaw and coastal erosion, are expected to have great impacts on the global climate system, on the ecosystem and on local communities. The magnitude at which these processes occur and their impacts is still not completely understood. This project focuses on the study of coastal erosion rates and the resulting organic carbon and nutrient release to the nearshore zone on Herschel Island and Yukon Coastal Plain in northwest Canada. The main aim is to explore means of coastal erosion, sediment transport to the sea and estimation of the amount of available organic

carbon and nutrients.

Background

Surface properties survey

Photos: M. Fritz, 2013

Soil organic carbon and nutrient release Soil organic carbon

and nutrient content map Rates of coastal erosion

Data mining

Ecological units Training data

Soil organic carbon and nutrient concentrations

Satellite imagery Surface properties

survey Core sampling

Laboratory CNS analysis

DEM comparison

LIDAR data Optical stereoparis

Data manipulation Field work

Laboratory work Geoprocessing

Referenzen

ÄHNLICHE DOKUMENTE

• highest rates of erosion → highest wave exposure and ice content. • Very high retreat rates (up to -4.0 m· a -1 )

The aim is to reveal di ff erences in total organic carbon (TOC), total carbon (TC) and total nitrogen (TN) between undisturbed (tundra zone, permafrost zone) and disturbed zones

PG2152 exhibit low organic carbon production and low TOC and TN content even in the top active layer although it shows the same soil conditions, no differences in elevation, type

Spits and beaches Wet polygonal terrain Hummocky tussock tundra Slightly disturbed uplands Alluvial fans. Moderately disturbed terrain Strongly

Hugues Lantuit, Michael Fritz, Birgit Heim, Lutz Schirrmeister, Veit Helm and Juliane

Coastal Permafrost Erosion (and carbon release).. Sediment/ Organic Carbon.

DOC fluxes from the erosion of massive ground ice at the coast seem to play only a minor role in the carbon budget as it is much lower than DOC fluxes from arctic rivers and fluxes

Training units and ground truth points were then defined on basis of vegetation, geomorphological and soil sur- veys performed in July 2013.. Samples were analysed for total