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Coring and compaction: Best practice in blue carbon stock and burial estimations
- Source :
- Geoderma. 364:114180
- Publication Year :
- 2020
- Publisher :
- Elsevier BV, 2020.
-
Abstract
- This work was supported by the Natural Environment Research Council (grant NE/R010846/1) Carbon Storage in Intertidal Environments (C-SIDE) project. A comparison of gouge and hammer coring techniques in intertidal wetland soils highlights a significant effect of soil compaction of up to 28% associated with the widely applied hammer coring method employed in Blue Carbon research. Hammer coring reduces the thickness of the soil profile and increases the dry bulk density, which results in an overestimation of the soil OC stock of up to 22%. In saltmarshes with multiple different soil units, we show that hammer coring is unsuitable for the calculation of OC stocks and should be avoided in favour of Russian or gouge cores. Compaction changes both soil dry bulk density and porosity and we show that resultant radiometric chronologies are compromised, almost doubling mass accumulation rates. While we show that the OC (%) content of these sediments is largely unchanged by coring method, the implication for OC burial rates are profound because of the significant effect of hammer coring on soil mass accumulation rates. Postprint
- Subjects :
- Compaction
Soil Science
Intertidal
Soil science
Environmental Science (miscellaneous)
010501 environmental sciences
01 natural sciences
law.invention
Hammer
Soil
law
Porosity
Earth-Surface Processes
0105 earth and related environmental sciences
Saltmarsh
Blue carbon
GE
Gouge
Sediment
DAS
04 agricultural and veterinary sciences
Bulk density
Coring
Age model
Soil water
040103 agronomy & agriculture
0401 agriculture, forestry, and fisheries
Environmental science
Soil horizon
GE Environmental Sciences
Subjects
Details
- ISSN :
- 00167061
- Volume :
- 364
- Database :
- OpenAIRE
- Journal :
- Geoderma
- Accession number :
- edsair.doi.dedup.....1002db9ac28e654bbb760d8719256de9
- Full Text :
- https://doi.org/10.1016/j.geoderma.2020.114180