Publication Date:
2022-08-12
Description:
Organic matter in soils of northern high latitudes show a high lability to recent permafrost thaw.
Mobilisation and release of soil organic matter (SOM) in permafrost areas might have a significant
impact on the carbon and nitrogen flux into the marine environment and in the atmosphere which
motivated scientists in the past to quantify carbon and nitrogen stocks. However, the determination
of environmental factors and their influences to SOM storage still need to be investigated more
accurately. This thesis seeks to contribute to an improvement of this issue.
This study investigates the SOM in the active layer and surficial permafrost on Herschel Island in
the western Canadian Arctic. It evaluates the preservation and degradation status of SOM in relation
to different landscape phenomena. To reach this goal, soil moisture, total organic carbon (TOC) and
total nitrogen (TN) contents were analysed on 128 samples from twelve sediment cores. The stable
carbon isotope (∂¹³C) composition on organic carbon and TOC/TN ratios (C/N) were determined.
Drilling locations were chosen based on of morphology, vegetation and soil properties and
supported by satellite imagery and air photos which classify the surface of Herschel Island into
seven ecological units. Regression analyses and principal component analysis (PCA) were used to
work out possible correlations and significant differences between environmental factors. Seasonal
thaw depths (active layer depths) increase with disturbance and a decreasing vegetation cover and
show depths between 20 and 100 cm. Results on organic matter show that consistently wellpreserved
SOM is accumulated in the active layer and subjacent ice-rich permafrost of depressional
polygonal tundra. Waterlogging leads to reduced organic matter decomposition and an enrichment
of the TOC and TN content characterising depressional polygonal tundra as a peatland environment.
Upland plateaus, gently rolling terrain and alluvial fans represent more than 50 % of the island and
show heterogeneous SOM storage characteristics with mostly considerable TOC contents being
limited to the active layer. SOM storage in subjacent permafrost is reduced. Disturbed areas with
slope gradients greater than 6° show strong SOM degradation with consistently low SOM contents
throughout the active layer and permafrost strata. Stabilised slopes show a reestablishment of a
vegetation cover and indicate initiation of SOM accumulation. This study highlights the
heterogeneity in SOM storage on Herschel Island which is mainly due to local morphology, soil
type, vegetation and moisture content. Principal component analysis shows that a gradient of
reduced SOM content is evident with increasing ground disturbance. Improved drainage decreases
the preservation of SOM in the active layer and ice rich permafrost can hold considerable SOM
contents. Future deepening of the active layer with increasing air temperatures in the Arctic might
remobilise SOM stored in ice-rich permafrost, especially in peatland environment.
Repository Name:
EPIC Alfred Wegener Institut
Type:
Thesis
,
NonPeerReviewed
Format:
application/pdf
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