Abstract
In Indonesia, tidal swampland is potential to be developed into agricultural land uses. Water management is the key success of farming on the tidal swampland. In the tidal swampland of Kalimantan, Indonesia, a fork irrigation system is widely applied in the water channels to supply irrigation water to the land. Besides irrigation, soil physical characteristics play an important role in controlling water availability for crops. The ability of soil to store water will determine the amount of available water that can be taken up by plants. This research aimed to determine the soil physical properties that are related to water availability in the soils from different land uses in a tidal swamp land area applied with a fork irrigation system. The experiment was conducted in dry season 2012, in Belawang, Barito Kuala district, South Kalimantan province. The soil samples were taken from four land uses, namely rice field, rubber plantation, mixed cropping, and unmanaged land. The soil physical properties, namely soil bulk density, particle density, porosity, texture, pF 1, pF 2, pF 2.54, pF 4, water content, total pore space, rapid drainage pores, slow drainage pores, available water, groundwater level were measured. In addition, the mineralogical properties of the soils were measured as well. The results showed that the physical properties of the soils taken from different land use varied, however, the change of the land use did not cause changes in the soil mineralogical properties. The mineralogy of the soils from different land uses are relatively the same, namely: quartz, illite, and chlorite.
Highlights
Natural phosphate rocks (PR) are an important natural material traditionally used for the production of P fertilizers
PH of PR’s from Sukabumi were significantly higher than that from Selagailingga when submerged with H2SO4 or CH3COOH (Table 3)
All of PR submerged with conventional solvent had significantly lower pH than that all agroindustrial wastewaters
Summary
Natural phosphate rocks (PR) are an important natural material traditionally used for the production of P (phosphorus) fertilizers. Traditional P fertilizer is produced based on chemical processing of a insoluble high-grade mineral phosphate which includes an energy intensively with sulfuric acid at a high temperature (Van Straaten 2002). This process is environmentally undesirable, it is not least because of the release of contaminants into the main product, gas streams and by-products. Phosphate rock is not available for plant where the soil pH is greater than 5.5-6.0 and even when conditions are optimal, plant yields are lower than those obtained with soluble phosphate (Khasawneh and Doll 1978).
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.