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Schirrmeister, Lutz; Siegert, Christine (2017): Pore-water analyses of permafrost deposits from Byk_98_MB-6.3 (Bykovsky Peninsula in 1998) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.881466, In supplement to: Schirrmeister, Lutz; Grigoriev, Mikhail N; Strauss, Jens; Grosse, Guido; Overduin, Pier Paul; Kohlodov, Aleksander; Guenther, Frank; Hubberten, Hans-Wolfgang (2018): Sediment characteristics of a thermokarst lagoon in the northeastern Siberian Arctic (Ivashkina Lagoon, Bykovsky Peninsula). arktos - The Journal of Arctic Geosciences, 4(1), https://doi.org/10.1007/s41063-018-0049-8

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Coverage:
Latitude: 71.807466 * Longitude: 129.351535
Date/Time Start: 1998-08-18T00:00:00 * Date/Time End: 1998-08-20T00:00:00
Event(s):
Byk_98_MB-6.3 * Latitude: 71.807466 * Longitude: 129.351535 * Date/Time Start: 1998-08-18T00:00:00 * Date/Time End: 1998-08-20T00:00:00 * Location: Lena Delta, Siberia, Russia * Campaign: RU-Land_1998_Lena (Lena-Delta1998) * Basis: AWI Arctic Land Expedition * Method/Device: Multiple investigations (MULT)
Comment:
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a proportionate amount of ultrapure water for a defined period of time. To obtain the water extracts, approximately 1 g of the freeze-dried sample was shaken for approximately 90 minutes in 50 ml centrifuge tubes with ultrapure water at a soil:water ratio of 1:25 using an overhead shaker (Gerhardt Laboshake). Then the suspension was centrifuged (Heraeus Multifuge 3s) at 4000 rpm for 15 minutes. The decanted extraction was filtered through a 0.45 µm cellulose acetate filter. We measured total dissolved elemental concentrations of Al, Ba, Ca, Fe, K, Mg, Mn, Na, P, Si, and Sr and anion concentrations of F-, Cl-, SO42-, Br-, NO3-, PO43-, and HCO3-.The element concentrations were analyzed using inductively coupled plasma-optical emission spectrometry (ICP-OES, Perkin-Elmer Optima 8300DV), while the anion content was determined by ion chromatography (IC, Thermo ICS2100). Hydrogen carbonate concentrations were measured by potentiometric pH-value titration with 0.01 M HCl using an automatic titrator (Metrohm 794 Basic Titrino). In order to estimate the procedural error, extractions were carried out in duplicate for every 5th to 10th sample and 2-3 blank solutions of ultrapure water were treated in the same manner as the extractions and measured for concentrations. Water EC and pH values were measured using a WTW MultiLab 540 multi-parameter device equipped with a TetraCon 325 cell referenced to 25 °C and a pH Sentix 81 electrode.
Size:
60 data points

Data

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Sample label

Height [m a.s.l.]

Sediment

pH

EC [µS/cm]

Al [µg/l]

Ca2+ [mg/l]

Fe [µg/l]

K+ [mg/l]
10 
Mg2+ [mg/l]
11 
Mn [mg/l]
12 
Na+ [mg/l]
13 
TP [mg/l]
14 
Si(OH)4 [µg/l]
15 
Sr2+ [µg/l]
16 
F- [µg/l]
17 
Cl- [mg/l]
18 
[NO3]- [mg/l]
19 
[SO4]2- [mg/l]
20 
[HCO3]- [mg/l]
MB-6.3-11.50silt6.3222.3213.320.71236.551.200.290.083882.00<0.106840.0000.660.000.527.63
MB-6.3-31.00silt6.6624.1154.341.4698.191.240.550.066740.80<0.106760.0000.330.001.698.42
MB-6.3-21.30silt6.5026.6186.941.47242.731.470.590.114211.04<0.107130.0000.700.000.978.79