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  • 2020-2024  (23)
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Keywords
Year
  • 1
    Publication Date: 2024-02-15
    Keywords: Analytical Balance, Sartorius, A200S; followed by Calulation; Arctic; Biomarkers; DATE/TIME; DEPTH, water; HER; Herschel_Island; LATITUDE; LONGITUDE; MULT; Multiple investigations; organic carbon; Permafrost; Sample code/label; Sample ID; Sample type; sediment; Size fraction; Zone
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2024-02-15
    Description: Particulate organic carbon (POC) and particulate organic nitrogen (PON) concentrations were obtained from water samples filtered on precombusted (450°C for 〉5 hours) 47mm Whatmann GF/F (0.7 µm) filters. The filters were dried overnight at 60°C and vacuum-sealed for storage in aluminum foil kept at -20°C until analysis. To determine POC and PON concentrations, the filters were acidified with 200-350 µl HCl 2N to remove carbonates, dried at 60°C overnight and then burned on a pre-calibrated CHN analyzer (Perkin Elmer, combustion at 925°C) for determination of the CO2 produced (Doxaran et al. 2012; doi:10.5194/bg-9-3213-2012).
    Keywords: 1_STN01; 1_STN020; 1_STN040; 1_STN0a; 1_STN0b; 1_STN140alt; 1_STN150alt; 1_STN340alt; 1_STN350; 1_STN360; 1_STN370alt; 1_STN380alt; 1_STN540alt; 1_STN550; 1_STN740; 1_STN810; 1_STN830; 1_STN840; 1_STN850; 1_STN860; 1_STN870; 2_STN030; 2_STN040; 2_STN1030; 2_STN1040; 2_STN1050; 2_STN1060; 2_STN110; 2_STN120; 2_STN140alt; 2_STN150alt; 2_STN310; 2_STN320; 2_STN330; 2_STN340alt; 2_STN350; 2_STN360; 2_STN370; 2_STN380alt_2; 2_STN420; 2_STN430; 2_STN450; 2_STN530; 2_STN540alt; 2_STN550; 2_STN565; 2_STN620; 2_STN630; 2_STN740; 2_STN800; 2_STN810; 2_STN820; 2_STN830; 2_STN840; 2_STN850; 2_STN860; 2_STN870; 2_STN999; 2_STNxxx; 2_XX2; 2_XX3; 3_STN010; 3_STN020; 3_STN030; 3_STN040; 3_STN1030; 3_STN1040; 3_STN1050; 3_STN1060; 3_STN125; 3_STN130; 3_STN130_5m; 3_STN135; 3_STN140alt; 3_STN150alt; 3_STN330; 3_STN340alt; 3_STN350; 3_STN360; 3_STN370alt; 3_STN380; 3_STN740; 3_STN800; 3_STN810; 3_STN820; 3_STN830; 3_STN840; 3_STN850; 3_STN860; 3_STN870; 3_STNR01; 3_STNR02; 3_STNR02_5m; 3_STNR03; 3_STNR04; 3_STNR05; 3_STNR06; 3_STNR07; 3_STNR08; 3_STNR09; 3_STNR09_20m; 3_STNR10; 3_STNR11; 3_STNR12; 3_STNR13; 3_STNxxx; 4_STN010; 4_STN020; 4_STN030; 4_STN040; 4_STN1030; 4_STN1040; 4_STN1050; 4_STN120; 4_STN125; 4_STN130; 4_STN135; 4_STN140alt; 4_STN140alt_2; 4_STN150alt; 4_STN330; 4_STN340alt; 4_STN350; 4_STN360; 4_STN370; 4_STN380alt; 4_STN740; 4_STN800; 4_STN810; 4_STN820; 4_STN830; 4_STN840; 4_STN840_2; 4_STN850; 4_STN860; 4_STN870; 4_STNR01; 4_STNR03; 4_STNR04; 4_STNR05; 4_STNR08; 4_STNR09; 4_STNR12; 4_STNXX4; 4_STNXX4_2; biogeochemistry; Biooptics; Carbon, organic, particulate; Carbon Hydrogen Nitrogen (CHN) analyzer (Perkin Elmer); Coastal waters; Cruise/expedition; DATE/TIME; DEPTH, water; Event label; hydrographic data; LATITUDE; LONGITUDE; Mackenzie; Mackenzie Delta, Canada; MULT; Multiple investigations; Nitrogen, organic, particulate; NUNATARYUK; NUNATARYUK, Permafrost thaw and the changing Arctic coast, science for socioeconomic adaptation; NunaWP4Mackenzie19_1_STN01; NunaWP4Mackenzie19_1_STN020; NunaWP4Mackenzie19_1_STN040; NunaWP4Mackenzie19_1_STN0a; NunaWP4Mackenzie19_1_STN0b; NunaWP4Mackenzie19_1_STN140alt; NunaWP4Mackenzie19_1_STN150alt; NunaWP4Mackenzie19_1_STN340alt; NunaWP4Mackenzie19_1_STN350; NunaWP4Mackenzie19_1_STN360; NunaWP4Mackenzie19_1_STN370alt; NunaWP4Mackenzie19_1_STN380alt; NunaWP4Mackenzie19_1_STN540alt; NunaWP4Mackenzie19_1_STN550; NunaWP4Mackenzie19_1_STN740; NunaWP4Mackenzie19_1_STN810; NunaWP4Mackenzie19_1_STN830; NunaWP4Mackenzie19_1_STN840; NunaWP4Mackenzie19_1_STN850; NunaWP4Mackenzie19_1_STN860; NunaWP4Mackenzie19_1_STN870; NunaWP4Mackenzie19_2_STN030; NunaWP4Mackenzie19_2_STN040; NunaWP4Mackenzie19_2_STN1030; NunaWP4Mackenzie19_2_STN1040; NunaWP4Mackenzie19_2_STN1050; NunaWP4Mackenzie19_2_STN1060; NunaWP4Mackenzie19_2_STN110; NunaWP4Mackenzie19_2_STN120; NunaWP4Mackenzie19_2_STN140alt; NunaWP4Mackenzie19_2_STN150alt; NunaWP4Mackenzie19_2_STN310; NunaWP4Mackenzie19_2_STN320; NunaWP4Mackenzie19_2_STN330; NunaWP4Mackenzie19_2_STN340alt; NunaWP4Mackenzie19_2_STN350; NunaWP4Mackenzie19_2_STN360; NunaWP4Mackenzie19_2_STN370; NunaWP4Mackenzie19_2_STN380alt_2; NunaWP4Mackenzie19_2_STN420; NunaWP4Mackenzie19_2_STN430; NunaWP4Mackenzie19_2_STN450; NunaWP4Mackenzie19_2_STN530; NunaWP4Mackenzie19_2_STN540alt; NunaWP4Mackenzie19_2_STN550; NunaWP4Mackenzie19_2_STN565; NunaWP4Mackenzie19_2_STN620; NunaWP4Mackenzie19_2_STN630; NunaWP4Mackenzie19_2_STN740; NunaWP4Mackenzie19_2_STN800; NunaWP4Mackenzie19_2_STN810; NunaWP4Mackenzie19_2_STN820; NunaWP4Mackenzie19_2_STN830; NunaWP4Mackenzie19_2_STN840; NunaWP4Mackenzie19_2_STN850; NunaWP4Mackenzie19_2_STN860; NunaWP4Mackenzie19_2_STN870; NunaWP4Mackenzie19_2_STN999; NunaWP4Mackenzie19_2_STNxxx; NunaWP4Mackenzie19_2_XX2; NunaWP4Mackenzie19_2_XX3; NunaWP4Mackenzie19_3_STN010; NunaWP4Mackenzie19_3_STN020; NunaWP4Mackenzie19_3_STN030; NunaWP4Mackenzie19_3_STN040; NunaWP4Mackenzie19_3_STN1030; NunaWP4Mackenzie19_3_STN1040; NunaWP4Mackenzie19_3_STN1050; NunaWP4Mackenzie19_3_STN1060; NunaWP4Mackenzie19_3_STN125; NunaWP4Mackenzie19_3_STN130; NunaWP4Mackenzie19_3_STN130_5m; NunaWP4Mackenzie19_3_STN135; NunaWP4Mackenzie19_3_STN140alt; NunaWP4Mackenzie19_3_STN150alt; NunaWP4Mackenzie19_3_STN330; NunaWP4Mackenzie19_3_STN340alt; NunaWP4Mackenzie19_3_STN350; NunaWP4Mackenzie19_3_STN360; NunaWP4Mackenzie19_3_STN370alt; NunaWP4Mackenzie19_3_STN380; NunaWP4Mackenzie19_3_STN740; NunaWP4Mackenzie19_3_STN800; NunaWP4Mackenzie19_3_STN810; NunaWP4Mackenzie19_3_STN820; NunaWP4Mackenzie19_3_STN830; NunaWP4Mackenzie19_3_STN840; NunaWP4Mackenzie19_3_STN850; NunaWP4Mackenzie19_3_STN860; NunaWP4Mackenzie19_3_STN870; NunaWP4Mackenzie19_3_STNR01; NunaWP4Mackenzie19_3_STNR02; NunaWP4Mackenzie19_3_STNR02_5m; NunaWP4Mackenzie19_3_STNR03; NunaWP4Mackenzie19_3_STNR04; NunaWP4Mackenzie19_3_STNR05; NunaWP4Mackenzie19_3_STNR06; NunaWP4Mackenzie19_3_STNR07; NunaWP4Mackenzie19_3_STNR08; NunaWP4Mackenzie19_3_STNR09; NunaWP4Mackenzie19_3_STNR09_20m; NunaWP4Mackenzie19_3_STNR10; NunaWP4Mackenzie19_3_STNR11; NunaWP4Mackenzie19_3_STNR12; NunaWP4Mackenzie19_3_STNR13; NunaWP4Mackenzie19_3_STNxxx; NunaWP4Mackenzie19_4_STN010; NunaWP4Mackenzie19_4_STN020; NunaWP4Mackenzie19_4_STN030; NunaWP4Mackenzie19_4_STN040; NunaWP4Mackenzie19_4_STN1030; NunaWP4Mackenzie19_4_STN1040; NunaWP4Mackenzie19_4_STN1050; NunaWP4Mackenzie19_4_STN120; NunaWP4Mackenzie19_4_STN125; NunaWP4Mackenzie19_4_STN130; NunaWP4Mackenzie19_4_STN135; NunaWP4Mackenzie19_4_STN140alt; NunaWP4Mackenzie19_4_STN140alt_2; NunaWP4Mackenzie19_4_STN150alt; NunaWP4Mackenzie19_4_STN330; NunaWP4Mackenzie19_4_STN340alt; NunaWP4Mackenzie19_4_STN350; NunaWP4Mackenzie19_4_STN360; NunaWP4Mackenzie19_4_STN370; NunaWP4Mackenzie19_4_STN380alt; NunaWP4Mackenzie19_4_STN740; NunaWP4Mackenzie19_4_STN800; NunaWP4Mackenzie19_4_STN810; NunaWP4Mackenzie19_4_STN820; NunaWP4Mackenzie19_4_STN830; NunaWP4Mackenzie19_4_STN840; NunaWP4Mackenzie19_4_STN840_2; NunaWP4Mackenzie19_4_STN850; NunaWP4Mackenzie19_4_STN860; NunaWP4Mackenzie19_4_STN870; NunaWP4Mackenzie19_4_STNR01; NunaWP4Mackenzie19_4_STNR03; NunaWP4Mackenzie19_4_STNR04; NunaWP4Mackenzie19_4_STNR05; NunaWP4Mackenzie19_4_STNR08; NunaWP4Mackenzie19_4_STNR09; NunaWP4Mackenzie19_4_STNR12; NunaWP4Mackenzie19_4_STNXX4; NunaWP4Mackenzie19_4_STNXX4_2; Station label
    Type: Dataset
    Format: text/tab-separated-values, 552 data points
    Location Call Number Expected Availability
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  • 3
    Publication Date: 2024-02-15
    Keywords: 3,5-dihydroxybenzoic acid/vanillyl phenols ratio; Acids/alkanes ratio; Age, 14C AMS; Age, dated; Arctic; Biomarkers; Calculated; Carbon, organic, total; Carbon/Nitrogen ratio; Carbon Preference Index, fatty acids; Carbon Preference Index, n-Alkanes; Cinnamyl phenols/vanillyl phenols ratio; Comment; Cutin, per unit mass organic carbon; Cutin/Lignin ratio; Elemental analyzer (EA), Thermo Scientific, FlashEA 1112; Fraction modern carbon; Fraction modern carbon, error, relative; Gas chromatograph (GC), Agilent, GC 7820; coupled with Quadrupole mass selective detector (MSD), Agilent, EI 5977B; HER; Herschel_Island; Isotope ratio mass spectrometry-elemental analyzer (IRMS-EA), Thermo Finnigan, Delta XP; Elemental analyzer (EA), Thermo Scientific, FlashEA 1112; Laboratory code/label; Lignin, per unit mass organic carbon; MICADAS accelerator mass spectrometer (AMS), Ionplus; according to McIntyre et al. (2017) and Haghipour et al. (2018); MULT; Multiple investigations; n-Alkane C23-33, high molecular weight, per unit mass organic carbon; n-Alkanoic acids C24-32, high molecular weight, per unit mass organic carbon; Nitrogen, total; organic carbon; p-coumaric acid/ferulic acid ratio; Permafrost; Sample ID; sediment; Syringic acid/syringaldehyde ratio; Syringyl phenols/vanillyl phenols ratio; Vanillic acid/vanillin ratio; Δ14C; δ13C
    Type: Dataset
    Format: text/tab-separated-values, 312 data points
    Location Call Number Expected Availability
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  • 4
    Publication Date: 2024-02-15
    Description: Collapse of permafrost coasts delivers large quantities of particulate organic carbon (POC) to arctic coastal areas. The objective of this study is to assess the pathways and fate of POC derived from thawing and eroding permafrost coasts in the nearshore zone, to better understand its impact on the carbon cycle and climate. We collected suspended particulate matter and sediment samples at the coastline and in the nearshore zone of Herschel Island - Qikiqtaruk (N 69.60°; W 139.00°) during a two‐week period in July‐August 2017. Locations were labelled A - H clockwise around the island, starting at the NE corner (Collinson Head). Samples were taken in transects perpendicular to the coast, at point locations offshore ('Monitoring point 1 - 3'), and from 'thaw streams', creeks carrying material from retrogressive thaw slumps and other abrupt thaw features, at various locations around the island. A total of 49 locations were visited; 12 at thaw streams, and 37 in the nearshore zone ranging from right at the shoreline to up to 20 m water depth (about 2 km offshore). We performed biogeochemical analyses (CN, δ13C, Δ14C) and sedimentological analyses (grain size, mineral surface area) in order to trace the pathway of permafrost material from its source to the nearshore water column and sediments.
    Keywords: Arctic; Coastal erosion; Nearshore zone; organic carbon; Permafrost
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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  • 5
    Publication Date: 2024-02-15
    Description: This study aims to give insight into the processes affecting permafrost organic carbon (OC) during transport from its source to its sink, through a study on three sediment fractions along a land-to-ocean transect. Material was followed from thawing permafrost, through a dynamic 'disturbed zone' and the nearshore zone, to an enclosed basin offshore Herschel Island - Qikiqtaruk, to assess sorting and degradation processes on specific fractions of sediment OC. Sediment, soil and permafrost samples were taken along a transect from the source (undisturbed active layer and permafrost), via two transitional zones (a terrestrial disturbed zone, i.e. the 'scar zone' of the RTS, and the marine nearshore zone up to a water depth of 5 m), to sink (basin sediment, water depth 〉20 m) at the coast of Herschel Island – Qikiqtaruk and the (semi-enclosed) Herschel Basin in Yukon, Canada, just west of the Mackenzie River delta. Samples were taken in May 2016 and July 2017. Sample material was fractionated with an aqueous (MilliQ) solution of sodium polytungstate (SPT; Na6[H2W12O40]), with a density of 1.8 g cm³, followed by wet-sieving over a 63 µm mesh, thus separating loose OC from mineral-associated OC. Each fraction was analysed for element content (TOC, TN), carbon isotopes (δ¹³C, Δ¹⁴C), molecular biomarkers (n-alkanes, n-alkanoic acids, lignin phenols, cutin acids), and mineral surface area. The relative abundance of specific biomarkers can also be used as indicator for degradation of organic carbon. Furthermore, the OC 'loading' (concentration of OC normalised to mineral surface area; in mgOC/m²) and terrestrial biomarker loading (µgOC/m²) can be used to assess loss of (permafrost) OC from mineral particles. The combination of these methods allows us to disentangle sorting processes from degradation of OC along the land-to-ocean continuum, and provides a detailed insight into the fate of thawed and eroded permafrost OC.
    Keywords: Arctic; Biomarkers; HER; Herschel_Island; MULT; Multiple investigations; organic carbon; Permafrost; sediment
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
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  • 6
    Publication Date: 2024-01-08
    Description: The aim of this project was to investigate nearshore depositional processes in the Arctic within the last century. For this study sediment cores were retrieved from lagoon and marine sites at Kanivaliuraq – Ptarmigan Bay (lagoon) and Herschel Basin (marine). The lagoon (YC18-PB-SC01, 64 cm length) and two marine (YC18-HB-GC01, 40 cm length; and PG2303-1, 20 cm length) sediment cores, were collected at 3, 18 and 43 m water depth, respectively. Sampling missions took place in April 2016 and August 2018 in the nearshore areas of the southern Beaufort Sea along the Yukon North Slope in the western Canadian Arctic. Lagoon core YC18-PB-SC01 was taken with a percussion corer and marine cores with an UWITEC gravity corer. The cores were kept cool and dark until further analysis in the laboratories. Mineralogy composition was obtained by X-ray diffraction (XRD) of bulk sediment (well ground and mixed) through a Siemens D500 X-Ray diffractometer and the spectra were resolved with EVA Bruker-AXS software. The grain size analysis results are presented in three groups, particles between 2 mm and 63 µm, 63 µm and 2 µm and smaller than 2 µm. All samples were treated with peroxide (30%) before laser diffraction to remove organic matter particles. Grain size analysis was performed using a Microtrac MRB's Bluewave and a Partica HORIBA laser diffraction device. The 210Pb activities were obtained by assuming a secular equilibrium with 210Po and using a spike of 209Po. Samples were digested by acid solutions (HNO3, HCl, HF and HNO3+H2O2). Both polonium radionuclides were deposited on a silver disk and measured by alpha spectrometry using ORTEC detectors coupled to MaestroTM data acquisition software. 226Ra and 137Cs activity were assessed by high-resolution gamma spectrometry through a germanium detector (ORTEC). The ages, mass and sediment accumulation rates (MAR and SAR, respectively) were inferred by a Constant Flux model also known as Constant Rate of Supply model. All uncertainties were calculated by Monte Carlo method.
    Keywords: Arctic Ocean; chronology; estuaries; Lagoon; marine sediments; mineralogy; Nearshore; Permafrost coasts
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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  • 7
    Publication Date: 2024-01-08
    Keywords: Accumulation rate, mass, per year; Accumulation rate, mass, per year, uncertainty; Age; Age, uncertainty; Albite; Alpha spectrometry quadratic propagation; Amphibole; Arctic Ocean; Caesium-137; Caesium-137, uncertainty; Calcite; Chlorite; chronology; Density, dry bulk; Density, dry bulk, uncertainty; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dolomite; Elapsed time; Elapsed time, uncertainty; estuaries; Gamma spectrometry quadratic propagation; Halite; Illite; Kaolinite; Lagoon; Lead-210; Lead-210, uncertainty; Lead-210 excess; Lead-210 excess, uncertainty; marine sediments; Mass per area; Mass per area, standard deviation; Microcline; mineralogy; Monte Carlo; Nearshore; PCOR; Percussion corer; Permafrost coasts; Pyrite, FeS2; Pyroxene; Quadratic propagation; Quartz; Radium-226; Radium-226, uncertainty; Sample code/label; Section; Sedimentation rate per year; Sedimentation rate per year, uncertainty; Size fraction 〈 0.002 mm, clay; Size fraction 〈 0.002 mm, clay, standard deviation; Size fraction 0.002-0.00063 mm; Size fraction 0.002-0.00063 mm, standard deviation; Size fraction 1.000-0.063 mm; Size fraction 1.000-0.063 mm, standard deviation; Smectite; South Beaufort Sea; YC18_PB_SCO1
    Type: Dataset
    Format: text/tab-separated-values, 1804 data points
    Location Call Number Expected Availability
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  • 8
    Publication Date: 2024-01-08
    Keywords: Albite; Alpha spectrometry quadratic propagation; Amphibole; Arctic Ocean; Caesium-137, activity per mass; Caesium-137, uncertainty; Calcite; Chlorite; chronology; Density, dry bulk; Density, dry bulk, uncertainty; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dolomite; Dry mass; Dry mass, standard deviation; estuaries; Gamma spectrometry quadratic propagation; GCUWI; Gravity corer, UWITEC; Halite; Illite; Kaolinite; Lagoon; Lead-210, uncertainty; Lead-210 activity per mass; Lead-210 excess; Lead-210 excess, uncertainty; marine sediments; Mass per area; Mass per area, standard deviation; Microcline; mineralogy; Nearshore; Permafrost coasts; Pyrite, FeS2; Pyroxene; Quadratic propagation; Quartz; Radium-226, uncertainty; Radium-226 activity per mass; Sample code/label; Section; Size fraction 〈 0.002 mm, clay; Size fraction 〈 0.002 mm, clay, standard deviation; Size fraction 0.002-0.00063 mm; Size fraction 0.002-0.00063 mm, standard deviation; Size fraction 1.000-0.063 mm; Size fraction 1.000-0.063 mm, standard deviation; Smectite; YC18_HB_GCO1
    Type: Dataset
    Format: text/tab-separated-values, 1272 data points
    Location Call Number Expected Availability
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  • 9
    Publication Date: 2024-01-08
    Keywords: Albite; Alpha spectrometry quadratic propagation; Amphibole; Arctic Ocean; Caesium-137; Caesium-137, uncertainty; Calcite; Chlorite; chronology; Density, dry bulk; Density, dry bulk, uncertainty; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dolomite; Dry mass; Dry mass, standard deviation; estuaries; Gamma spectrometry quadratic propagation; GCUWI; Gravity corer, UWITEC; Halite; Illite; Kaolinite; Lagoon; Lead-210; Lead-210, uncertainty; Lead-210 excess; Lead-210 excess, uncertainty; marine sediments; Mass per area; Mass per area, standard deviation; Microcline; mineralogy; Nearshore; Permafrost coasts; PG2303_1; Pyrite, FeS2; Pyroxene; Quadratic propagation; Quartz; Radium-226; Radium-226, uncertainty; Sample code/label; Section; Size fraction 〈 0.002 mm, clay; Size fraction 〈 0.002 mm, clay, standard deviation; Size fraction 0.002-0.00063 mm; Size fraction 0.002-0.00063 mm, standard deviation; Size fraction 1.000-0.063 mm; Size fraction 1.000-0.063 mm, standard deviation; Smectite; South Beaufort Sea
    Type: Dataset
    Format: text/tab-separated-values, 767 data points
    Location Call Number Expected Availability
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  • 10
    Publication Date: 2024-03-01
    Keywords: Age, 14C AMS; Age, dated; Arctic; Biomarkers; Calculated; Carbon, organic, total; Carbon/Nitrogen ratio; Comment; Elemental analyzer (EA), Thermo Scientific, FlashEA 1112; Fraction modern carbon; Fraction modern carbon, error, relative; HER; Herschel_Island; Isotope ratio mass spectrometry-elemental analyzer (IRMS-EA), Thermo Finnigan, Delta XP; Elemental analyzer (EA), Thermo Scientific, FlashEA 1112; Laboratory code/label; MICADAS accelerator mass spectrometer (AMS), Ionplus; according to McIntyre et al. (2017) and Haghipour et al. (2018); Minerals, surface area; MULT; Multiple investigations; Nitrogen, total; organic carbon; Organic carbon, loading; Permafrost; Sample ID; sediment; Surface area analyzer, Quantachrome, Nova 4200e; 6-point Brunauer–Emmett–Teller (BET) method according to Brunauer et al. (1938); Δ14C; δ13C
    Type: Dataset
    Format: text/tab-separated-values, 161 data points
    Location Call Number Expected Availability
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