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  • 1
    Monograph available for loan
    Monograph available for loan
    San Francisco : Freeman, Cooper & Co.
    Call number: G 8050
    Type of Medium: Monograph available for loan
    Pages: 397 S. : Ill.
    ISBN: 0877353212
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Call number: AWI G1-19-92268
    In: University of California publications in geological sciences, Volume 85
    Type of Medium: Monograph available for loan
    Pages: V, 101 Seiten , Illustrationen
    Series Statement: University of California publications in geological sciences 85
    Language: English
    Note: Contents: Abstract. - Introduction and Acknowledgements. - Metamorphic basement. - Plutonic rocks. - Review of plutonism in Central America, excluding Honduras. - Plutonic rocks of Honduras. - Mesozoic and eocene rocks. - General statement. - Vallę de Angeles group. - Esquias formation. - Matagalpa Formation. - Subinal redbeds. - Ignimbrites. - The pre-ignimbrite surface. - Thickness of the ignimbrites. - Lithology and mineral composition. - Associated lavas. - Ignimbrite vents. - Fluviatile and lacustrine beds associated with ignimbrites. - Age and correlation. - Chemical composition - major elements. - Origin of ignimbrite magmas. - Dikes. - Borderlands of the Gulf of Fonseca. - The Gracias Formation. - Quaternary Volcanism. - General statement. - Description of individual volcanic fields. - Gulf of Fonseea. - Volcanoes of the central highlands. - The Lake Yojoa volcanic field. - Lavas in the Sula graben. - Utila Island. - Geologic structure of Honduras. - Appendix: Microscopic Petrography. - A. Plutonic rocks. - B. Andesites and basalts of the Matagalpa Formation. - C. Lavas of the Gulf of Fonseca sequence. - D. Dike rocks. - E. Ignimbrites. - F. Quaternary lavas. - Literature cited.
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 3
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    PANGAEA
    In:  Supplement to: Cobb, Alexander R; Harvey, Charles Franklin (2019): Scalar Simulation and Parameterization of Water Table Dynamics in Tropical Peatlands. Water Resources Research, 55(11), 9351-9377, https://doi.org/10.1029/2019WR025411
    Publication Date: 2023-01-13
    Description: doi:10.1594/PANGAEA.908215: This collection of datasets provides the water table and throughfall data from Brunei Darussalam used in the paper: Scalar simulation and parameterization of water table dynamics in tropical peatlands by Alexander R. Cobb and Charles F. Harvey (Water Resources Research 55, doi:10.1029/2019WR025411; Cobb and Harvey 2019). It additionally provides the parameters for the peat hydraulic conductivity and specific yield functions derived in the paper, and the topographic data used to calculate the two-dimensional Laplacian of the peatsurface elevation. doi:10.1594/PANGAEA.908211: The flowtube described in this flowtube geometry dataset encloses the piezometers and througfall gauges. The centroid of the throughfall gauges is taken as the location of the flowtube (in the location dataset). The areas and integrated gradients provided in the flowtube geometry dataset were used to calculate the two-dimensional Laplacian of the peat surface elevation, used in Cobb and Harvey (2019). doi:10.1594/PANGAEA.908209: The hydraulic conductivity knots are recorded along with their 95% confidence intervals. Details on how they were computed from the peat surface Laplacian and throughfall and water table time series are provided in Cobb and Harvey (2019). doi:10.1594/PANGAEA.908210: The specific yield knots are recorded along with their 95% confidence intervals. Details on how they were computed from the peat surface Laplacian and throughfall and water table time series are provided inCobb and Harvey (2019). doi:10.1594/PANGAEA.908214: The throughfall data are the average of data from four siphoning tipping-bucket rain gauges (Texas Electronics TR-525S, Dallas, Texas, USA) installed 50 cm above the peat surface along a 100 m transect, as described in Cobb and Harvey (2019). The coordinates provided for the throughfall measurements (in locations dataset) are the coordinates of the mid-point of the 4 throughfall gauges. The coordinates of the individual throughfall gauges were: Gauge 1: 114.354260, 4.370139 Gauge 2: 114.354034, 4.369900 Gauge 3: 114.353943, 4.369769 Gauge 4: 114.353661, 4.369449 The centroid of these 4 locations (recorded in locations dataset) was found by converting the coordinates of each gauge to a local projected coordinate system (GDBD2009, EPSG:5247), averaging the northing and easting coordinates, and converting back to longitude-latitude coordinates (EPSG:4326).
    Keywords: hydraulic conductivity; specific yield; throughfall; tropical peat swamp; water table
    Type: Dataset
    Format: application/zip, 8 datasets
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  • 4
    Publication Date: 2023-01-13
    Description: The hydraulic conductivity knots are recorded along with their 95% confidence intervals. Details on how they were computed from the peat surface Laplacian and throughfall and water table time series are provided in Cobb and Harvey (2019).
    Keywords: hydraulic conductivity; Hydraulic conductivity; Model calibration; Solinst Levelogger; specific yield; throughfall; tropical peat swamp; Water level; water table
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 5
    Publication Date: 2023-01-13
    Description: Water level data were obtained from logging pressure transducers (Solinst Levelogger Edge 3001, Solinst Canada, Georgetown, Ontario, Canada) corrected for barometeric fluctuations using a barometer (Solinst Barologger Gold 3001). Each transducer was suspended on a steel cable inside a 2" PVC pipe 1.5 m in length installed to 1.4 m depth and screened at 1.3--1.45 m below the top of the piezometer casing. Piezometers were developed prior to measurement by repeatedly plunging and removing a solid rod into the piezometer tube. The details of how the surface datum was obtained are described in Cobb et al (2017, doi:10.1073/pnas.1701090114).
    Keywords: Brunei_Darussalam_mdm_trail_7; DATE/TIME; hydraulic conductivity; Solinst Levelogger; specific yield; throughfall; tropical peat swamp; Water level; water table
    Type: Dataset
    Format: text/tab-separated-values, 25790 data points
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  • 6
    Publication Date: 2023-01-13
    Description: Water level data were obtained from logging pressure transducers (Solinst Levelogger Edge 3001, Solinst Canada, Georgetown, Ontario, Canada) corrected for barometeric fluctuations using a barometer (Solinst Barologger Gold 3001). Each transducer was suspended on a steel cable inside a 2" PVC pipe 1.5 m in length installed to 1.4 m depth and screened at 1.3--1.45 m below the top of the piezometer casing. Piezometers were developed prior to measurement by repeatedly plunging and removing a solid rod into the piezometer tube. The details of how the surface datum was obtained are described in Cobb et al (2017, doi:10.1073/pnas.1701090114).
    Keywords: Brunei_Darussalam_mdm_trail_10; DATE/TIME; hydraulic conductivity; Solinst Levelogger; specific yield; throughfall; tropical peat swamp; Water level; water table
    Type: Dataset
    Format: text/tab-separated-values, 25790 data points
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  • 7
    Publication Date: 2023-01-13
    Description: The flowtube described in this flowtube geometry dataset encloses the piezometers and througfall gauges. The centroid of the throughfall gauges is taken as the location of the flowtube (in the location dataset). The areas and integrated gradients provided in the flowtube geometry dataset were used to calculate the two-dimensional Laplacian of the peat surface elevation, used in Cobb and Harvey (2019).
    Keywords: Area; Brunei_Darussalam; hydraulic conductivity; Integrated normal gradient; specific yield; throughfall; tropical peat swamp; water table
    Type: Dataset
    Format: text/tab-separated-values, 192 data points
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  • 8
    Publication Date: 2023-01-13
    Description: This dataset contains raster grids in GeoTIFF format describing the constraints on accumulation of tropical peat imposed by drainage network geometry in regions of northwest and southern Borneo. Each raster in the dataset gives the geometric capacity for peat accumulation (non-dimensional equilibrium peat thickness) in a parcel of land, calculated using the method described in the paper. The parcels are grouped into five areas, referred to by the names Badas, Baram, Belait, EMRP and Sebangau. Rasters have arbitrary numeric labels (001.tif, 002.tif, ...) in all areas except the Badas area, where descriptive names are used for the parcels before (badas) and after (badas_west and badas_east) subdivision by a canal. The map projection and resolution are included in each raster via standard GeoTIFF metadata; the projections used were EPSG:5247 for the Badas, Baram, and Belait areas and EPSG:32749 for the EMRP and Sebangau areas.
    Keywords: drainage networks; land use impacts; peatland carbon storage; peatland drainage; Tropical peatlands
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 9
    Publication Date: 2023-01-13
    Description: Water level data were obtained from logging pressure transducers (Solinst Levelogger Edge 3001, Solinst Canada, Georgetown, Ontario, Canada) corrected for barometeric fluctuations using a barometer (Solinst Barologger Gold 3001). Each transducer was suspended on a steel cable inside a 2" PVC pipe 1.5 m in length installed to 1.4 m depth and screened at 1.3--1.45 m below the top of the piezometer casing. Piezometers were developed prior to measurement by repeatedly plunging and removing a solid rod into the piezometer tube. The details of how the surface datum was obtained are described in Cobb et al (2017, doi:10.1073/pnas.1701090114).
    Keywords: Brunei_Darussalam_mdm_trail_8; DATE/TIME; hydraulic conductivity; Solinst Levelogger; specific yield; throughfall; tropical peat swamp; Water level; water table
    Type: Dataset
    Format: text/tab-separated-values, 25789 data points
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  • 10
    Publication Date: 2023-01-13
    Description: Water level data were obtained from logging pressure transducers (Solinst Levelogger Edge 3001, Solinst Canada, Georgetown, Ontario, Canada) corrected for barometeric fluctuations using a barometer (Solinst Barologger Gold 3001). Each transducer was suspended on a steel cable inside a 2" PVC pipe 1.5 m in length installed to 1.4 m depth and screened at 1.3--1.45 m below the top of the piezometer casing. Piezometers were developed prior to measurement by repeatedly plunging and removing a solid rod into the piezometer tube. The details of how the surface datum was obtained are described in Cobb et al (2017, doi:10.1073/pnas.1701090114).
    Keywords: Brunei_Darussalam_mdm_trail_6; DATE/TIME; hydraulic conductivity; Solinst Levelogger; specific yield; throughfall; tropical peat swamp; Water level; water table
    Type: Dataset
    Format: text/tab-separated-values, 25790 data points
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