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Oskarsdottir, Sigrídur Magnea; Gislason, Sigurdur Reynir; Snorrason, Arni; Halldorsdottir, Stefanía Gudrún; Gisladottir, Gudrún (2011): (Supplement 1) Selected chemical composition of Icelandic river waters and bedrock age [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.818182, Supplement to: Oskarsdottir, SM et al. (2011): Spatial distribution of dissolved constituents in Icelandic river waters. Journal of Hydrology, 397(3-4), 175-190, https://doi.org/10.1016/j.jhydrol.2010.11.028

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Abstract:
In this study we map the spatial distribution of selected dissolved constituents in Icelandic river waters using GIS methods to study and interpret the connection between river chemistry, bedrock, hydrology, vegetation and aquatic ecology. Five parameters were selected: alkalinity, SiO2, Mo, F and the dissolved inorganic nitrogen and dissolved inorganic phosphorus mole ratio (DIN/DIP). The highest concentrations were found in rivers draining young rocks within the volcanic rift zone and especially those draining active central volcanoes. However, several catchments on the margins of the rift zone also had high values for these parameters, due to geothermal influence or wetlands within their catchment area. The DIN/DIP mole ratio was higher than 16 in rivers draining old rocks, but lowest in rivers within the volcanic rift zone. Thus primary production in the rivers is limited by fixed dissolved nitrogen within the rift zone, but dissolved phosphorus in the old Tertiary catchments. Nitrogen fixation within the rift zone can be enhanced by high dissolved molybdenum concentrations in the vicinity of volcanoes.
The river catchments in this study were subdivided into several hydrological categories. Importantly, the variation in the hydrology of the catchments cannot alone explain the variation in dissolved constituents. The presence or absence of central volcanoes, young reactive rocks, geothermal systems and wetlands is important for the chemistry of the river waters. We used too many categories within several of the river catchments to be able to determine a statistically significant connection between the chem¬istry of the river waters and the hydrological categories. More data are needed from rivers draining one single hydrological category. The spatial dissolved constituent distribution clearly revealed the difference between the two extremes, the young rocks of the volcanic rift zone and the old Tertiary terrain.
Coverage:
Median Latitude: 64.656554 * Median Longitude: -18.730571 * South-bound Latitude: 63.420000 * West-bound Longitude: -23.170000 * North-bound Latitude: 66.174000 * East-bound Longitude: -14.000000
Event(s):
IS_A-Jokulsa (V144)  * Latitude: 65.277000 * Longitude: -18.797000 * Location: Iceland * Method/Device: Water sample (WS)
IS_Asa-Eldvatn (V328)  * Latitude: 63.643000 * Longitude: -18.338000 * Location: Iceland * Method/Device: Water sample (WS)
IS_Blanda (V54)  * Latitude: 65.409000 * Longitude: -19.735000 * Location: Iceland * Method/Device: Water sample (WS)
Comment:
Positions approximate. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
Latitude of eventLatitude
Longitude of eventLongitude
Station labelStationOskarsdottir, Sigrídur Magnea
Age, mineralAge mineralMaOskarsdottir, Sigrídur Magneawt age of bedrock
Silicon dioxideSiO2mol/kgOskarsdottir, Sigrídur Magnea
Alkalinity, totalATmmol(eq)/kgOskarsdottir, Sigrídur Magneaunit meq/kg
MolybdenumMonmol/kgOskarsdottir, Sigrídur Magnea
FluorineFµmol/kgOskarsdottir, Sigrídur Magnea
10 Nitrogen, inorganic, dissolved/Phosphorus, inorganic, dissolved ratioDIN/DIPOskarsdottir, Sigrídur MagneaCalculated, ratio of molar masses
Size:
335 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

Latitude

Longitude

Station

Age mineral [Ma]

SiO2 [mol/kg]

AT [mmol(eq)/kg]

Mo [nmol/kg]

F [µmol/kg]
10 
DIN/DIP
IS_A-Jokulsa 65.277-18.797V1442.300.00017100.2751.2002.9501.797
IS_Asa-Eldvatn 63.643-18.338V3280.070.00027900.6802.7107.59121.960
IS_Blanda 65.409-19.735V540.820.00016400.4132.4003.4909.388
IS_Bruara 64.231-20.455V1080.230.00021900.3380.8802.7505.580
IS_Djupa 63.924-17.579V1500.720.00030700.3074.2503.057
IS_Dynjandi 65.695-23.133V1911.750.00007000.050
IS_Eldvatn_M 63.612-18.149V3300.030.00031700.6744.14010.8002.680
IS_Ellidaar 64.062-21.762V3010.270.00014000.4680.7662.3105.440
IS_Fellsa 64.876-15.013V2065.870.00012300.2180.5601.03020.790
IS_Fjardará 65.223-14.000V285611.750.00009600.1530.2000.70622.270
IS_Fljótsdal 64.943-15.039V1091.620.00011100.4992.9803.19011.790
IS_Flokadalsa 64.579-21.441V40172.190.00022400.4152.59074.800
IS_Fnjoska 65.815-17.869V2000.840.00026000.4131.3500.700
IS_Geithellnaa 64.587-14.763V2775.389.880
IS_Gigja 63.911-17.275V1590.000.00012700.4977.7603.120
IS_Grenlaekur 63.699-17.875V3390.550.00030600.6483.8408.6901.820
IS_Grimsa_L 64.555-21.523V40152.550.00020900.5252.92057.960
IS_Grimsa_S 65.101-14.479V1065.500.00015400.3380.8601.61019.160
IS_Grimsstadir 65.593-16.150V1020.180.00020900.8115.6107.0661.187
IS_Hamarsa 64.654-14.543V1025.437.310
IS_Hjaltadalsa 65.763-19.241V5111.400.00019000.1602.270
IS_Hjardarhagi 65.315-14.951V1101.010.00009700.3331.2401.9106.770
IS_Hverfisfljot 63.873-17.652V714.780.00017400.3632.2003.9203.001
IS_Hvita_S 64.229-20.128V40130.410.00020300.5462.7005.4102.930
IS_Hvita_W 64.639-21.463V660.800.00019600.4303.00812.810
IS_Kaldakvisl 64.400-18.550V2520.940.00006870.7206.3105.390
IS_Kreppa 64.995-16.119V1630.070.00013800.4423.6841.460
IS_Laqarfliot 65.467-14.371V174.740.00014400.4091.2201.76010.940
IS_Laxa_A 65.559-17.080V1051.700.00022001.2008.38012.3002.940
IS_Laxa_V 64.368-21.811V40205.530.00036300.3601.61074.080
IS_Leira 63.601-18.531V12030.100.00021300.86013.44016.300
IS_Langisjór 64.188-18.112V4010.200.00007600.4091.2602.7105.070
IS_Loni 64.401-14.876V26053.442.540
IS_Mulakvisl 63.420-18.796V890.140.00030101.17925.7906.755
IS_Nordura 64.675-21.556V1285.420.00018100.3381.4401.4609.570
IS_Olfusa 63.894-20.922V640.680.00021300.4572.1604.6209.320
IS_Osa 66.107-23.170V26399.200.00008000.149
IS_Reykjadalsa 64.608-21.454V40163.850.00040000.62010.86094.710
IS_Sanda 66.174-15.542V263.210.00056500.346
IS_Skaftárdalur 63.759-18.434V700.220.00023700.6062.3205.6105.090
IS_Skeidará 63.951-16.908V880.260.00021202.03611.86011.130
IS_Skjálfandafljót 65.344-17.309V2380.780.00021600.5194.91010.400
IS_Skötufjardara 65.849-22.792V40211.000.00007000.124
IS_Sog 64.030-20.937V2710.300.00018200.4721.4803.6806.870
IS_Sula 63.929-17.377V22010.210.00015000.4974.7306.080
IS_Thjorsa_U 63.897-20.580V3200.530.00021000.5704.1008.6002.960
IS_Thvera_N 64.651-21.370V40145.340.00013900.4553.86056.830
IS_Thvera_S 64.414-21.472V40194.040.00013000.3401.86069.350
IS_Tungnaa 64.252-18.196V980.83
IS_Tungufljot 64.203-20.289V680.450.00025900.3641.8603.6205.630
IS_Vatnsdalsa 65.264-20.034V451.640.00034800.6802.3004.2504.070
IS_Vatnsdalsa_B 65.557-23.074V20411.320.00003000.070
IS_Vesturkvisl 64.187-18.054V4700.03
IS_Vididalsa 65.294-20.545V4683.260.00030800.6412.3709.990
IS_W-Jokulsa 65.285-19.034V1451.530.00026300.6752.4006.0400.031
IS_Ytri-Ranga 63.836-20.264V3210.170.00029001.28718.07028.0702.150