The doi above is for this specific version of this dataset, which is currently the latest. Newer versions may be published in the future. For a link that will always point to the latest version, please use
doi: 10.4121/16947889

Novi Rahmawati; Deasy Arisanty; Dedi Rosadi (2022): Supplementary data for paper: Soil Physical Characteristics and Saturated Hydraulic Conductivity in the Landform of Barito Delta, Kalimantan, Indonesia. Version 4. 4TU.ResearchData. dataset. https://doi.org/10.4121/16947889.v4

Dataset

x choose version: version 3 - 2022-01-11 version 2 - 2021-11-22 version 1 - 2021-11-11

• Ecological Applications
• Environmental Science and Management
• Physical Geography and Environmental Geoscience
• Other Earth Sciences

barito delta, bulk density, landform, saturated hydraulic conductivity, soil fraction, soil profile, soil texture

view on openstreetmap

2011 and 2022

CC BY 4.0

RefWorks, BibTeX, Reference Manager, Endnote, DataCite, NLM, DC, CFF

by Novi Rahmawati , Deasy Arisanty , Dedi Rosadi

This data contain soil textures, bulk density, soil organic matter, saturated hydraulic conductivity, landform map, soil sample location map, electrical ressistivity measurement location, and soil profile location. Soil samples are taken in each depth of soil until 5 m depth. The sample is taken representatively in every landforms in Barito Delta. Soil sample is not taken until 5 m depth in case it found fine sand material. It is because this sand material is from ancient sedimentation that occured in the past. The sample is not taken in Oxbow Lake because it is mostly covered with grass land and water. Particle size distribution (% clay, % silt and % silt) is defined from laboratory testing. USDA triangle texture is used to determine soil texture. Bulk density is sampled in land surface only or at 1 meter depth since the value is almost homogenous in peatland. Soil organic matter (SOM) is sampled similar way with soil texture. Soil profile location is used to characterize soil texture in each depth of each landform in Barito Delta. Bayesian statistics is used to interpolate soil fraction in each depth to derive soil fraction map in each soil profile location. Saturated hydraulic conductivity is estimated from every sample and every depth applying Saxton and Raws (1986) and (2006), Weynants et al (2009) formulas. Research objective is to characterize soil fraction, soil texture, soil organic matter, and saturated hydraulic conductivity in peatland of Barito delta where get influence from river and sea sedimentation. Soil sample for soil texture, soil organic matter, bulk density and electrical resistivity measurement are primary data. Landform is mapped using fieldcheck in 2011 of land use from landsat year 2008; soil map from institution scale 1:250,000; and topography map scale 1: 250,000

• 2021-11-11 first online

• 2022-04-07 published, posted

4TU.ResearchData

tiff, xml, excel, shp

Soil Physical Characteristics and Saturated Hydraulic Conductivity in the Landform of Barito Delta, Kalimantan, Indonesia

• Lambung Mangkurat University for open access article

University of Twente, Faculty of Geo-information Science and Earth Observation (ITC), Department of Water Resources