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All Journal Agromet DIKSI Journal of Tropical Soils Jurnal Sumberdaya Lahan BERITA BIOLOGI Jurnal Sumberdaya Lahan Jurnal Pendidikan Madrasah Al-Fathin: Jurnal Bahasa dan Sastra Arab International Journal of Arabic Language Teaching IJALT Akrab Juara : Jurnal Ilmu-ilmu Sosial Bulletin of Community Engagement Uktub: Journal of Arabic Studies Edukasia: Jurnal Pendidikan dan Pembelajaran Jurnal Pengabdian Pada Masyarakat Qismul Arab: Journal of Arabic Education
Ani Susilawati
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Journal : Journal of Tropical Soils

 1 
Physical Properties of Soils from Several Land Uses in a Tidal Swampland Area Applied with a Fork Irrigation System Susilawati, Ani; Nursyamsi, Dedi; Syahbuddin, Haris
JOURNAL OF TROPICAL SOILS Vol. 22 No. 3: September 2017
Publisher : UNIVERSITY OF LAMPUNG

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.5400/jts.2017.v22i3.167-174

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. 
Changes of Soil Chemical Properties during Rice Straw Decomposition in Different Types of Acid Sulphate Soils Hairani, Anna; Susilawati, Ani
JOURNAL OF TROPICAL SOILS Vol. 18 No. 2: May 2013
Publisher : UNIVERSITY OF LAMPUNG

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.5400/jts.2013.v18i2.99-103

Abstract

Organic residues often exhibit different physico-chemical properties and affect the soil ecosystem in different ways. Hence, the study of their impact on soil is essential to benefit from their potential as amendments and to avoid adverse environmental effects. It is required to study the role of rice straw in the changes of soil properties during decomposition processes in the rice field. The research was conducted on potential acid sulphate soil (PASS) and actual acid sulphate soil (AASS) in the glass house. Soil pH, Fe2+, organic-Fe, total N and available P were observed at 2, 4, 6 and 8 weeks after planting (WAP). The result showed that rice straw application : (1) decreased soil pH of PASS and increase soil pH of AASS; (2) tended to increase Fe2+ both in PASS and AASS; (3) stimulated the organic-Fe concentration in AASS was higher than organic-Fe concentration in PASS; (4) had no different effect in total N and decreased P concentration in the both of soil during observation. P concentration on PASS was lower than on AASS.Keywords: Decomposition, rice straw, soil chemical properties, soil type[How to Cite: Hairani A and A Susilawati. 2013.Changes of Soil Chemical Properties during Rice Straw Decomposition in Different Types of Acid Sulphate Soils. J Trop Soils 18 (2): 99-103. Doi: 10.5400/jts.2013.18.2.99]REFERENCESBalai Penelitian Tanah. 2005. Analisis Kimia Tanah, Tanaman, Air dan Pupuk.  Badan Penelitian dan Pengembangan Pertanian. Departemen Pertanian.  Bogor. p: 136 (in Indonesian).Banach AM, K Banach, RCJH Peters,  RHM Jansen, EJW Visser, Z Stepniewska, JGM Roelofs and LPM Lamers.  2009.  Effects of long-term flooding on biogeochemistry and vegetation development in floodplains; a mesocosm experiment to study interacting effects of land use and water quality.  Biogeosciences  6: 1325-1339. doi:10.5194/bg-6-1325-2009.Bonneville S.  2005.  Kinetics of Microbial Fe (III) Oxyhydroxide Reduction : The Role of Mineral Properties.  [Dissertation].  Department of Earth Sciences-Geochemistry, Faculty of Geosciences, Utrecht University. The Netherlands. 117 p.Cayuela ML, T Sinicco and C Mondini.  2009.  Mineralization dynamics and biochemical properties during initial decomposition of plant and animal residues in soil. App Soil Ecol  41: 118 -127.De-Campos AB, AL Mamedov and C Huang. 2009. Short-term reducing conditions decrease soil aggregation. Soil Sci Soc Am J  73: 550-559.Dent D. 1986. Acid Sulphate Soils: A Baseline for Research and Development. International Land Reclamation Institute Pub. 39. Wageningen, The Netherlands. 204 p.Dobermann A and T Fairhurst.  2000.  Rice: Nutrient Disorders and Nutrient Management.  International Rice Research Institute.  Makati city, The Fhillipines.  191 p. Fahmi A, B Radjagukguk and BH Purwanto.  2009.  Kelarutan posfat dan ferro pada tanah sulfat masam yang diberi bahan organik jerami padi.  J Tanah Trop 14: 119 -125 (in Indonesian).Fahmi A. 2010.  Pengaruh pemberian jerami padi terhadap pertumbuhan tanaman padi (Oryza sativa ) di tanah sulfat masam.  J Berita Biol 10:  7-14 (in Indonesian). Havlin JL, JD Beaton, SL Tisdale and WL Nelson. 2005. Soil Fertility and Fertilizers, an introduction to nutrient management. 7th edition. Prentice Hall. 515 p.Indrayati L and A  Jumberi. 2002.  Pengelolaan jerami padi pada pertanaman padi di lahan pasang surut sulfat masam.  In: Pengelolaan Tanaman Pangan Lahan Rawa.  Badan Penelitian dan Pengembangan Pertanian, Puslitbang Tanaman Pangan, Bogor. Kirk G.  2004.  The Biogeochemistry of Submerged Soils. John Willey and Sons. Chicester, England.  291 p.Kongchum M.  2005.  Effect of  Plant Residue and Water Management Practices on Soil Redox Chemistry, Methane Emission and Rice Productivity.   [Dissertation].  Graduate Faculty of the Louisiana State University.  USA.  201 pKyuma K.  2004.  Paddy Soil Science.  Kyoto University Press dan Trans Pacific Press.  Melbourne.  Australia. 279 p.Liang X, J Liu, Y Chen, H Li, Y Ye, Z Nie, M Su and Z Xu.  2010.  Effect of pH on the release of soil colloidal phosphorus.  J Soils Sediments 10: 1548-1556.Lindsay WL. 1979.  Chemical Equilibria in Soils. John Willey & Sons. New York. 449 p.Liu C, M Chen and F Li. 2010. Fe(III) reduction in soils from South China. In: RJ Gilkes and N Prakongkep (eds). Soil Solutions for a Changing World. Soil minerals and contaminants, 19th World Congress of Soil Science. Brisbane, Australia, pp.70-73.McIntyre RES, MA Adams, DJ Ford and PF Grierson.  2009.  Rewetting and litter addition influence mineralization and microbial communities in soils from a semi-arid intermittent stream.  Soil Biol Biochem 41: 92-101.Morris AJ. 2011. Phosphate Binding to Fe and Al in Organic Matter as Affected by Redox Potential and pH. [Dissertation]. Soil Science, North Carolina  State University, Raleigh, North Carolina, USA. 229 p.Olomu MO, GJ Racz and CM Cho.  1973.  Effect of flooding on the Eh, pH, and concentrations of Fe and Mn in several manitoba soils.  Soil Sci Soc Am J  37: 220 -224.Ponnamperuma FN. 1984.  Effects of flooding on soils.  In: T Kozlawski (ed).  Flooding and Plant Growth: Physical Ecology. A Series Monographs, Text and Treatises.  Academic Press Inc.  Harcourt Brace Javanovich Publisher, USA, pp. 10-45. Reddy KR and RD Delaune.  2008. The Biogeochemistry of Wetland; Science and Application. CRC Press.  New York.Rukhsana F, C Butterly, J Baldock and C Tang.  2010. Model carbon compounds differ in their effects on pH change of soils with different initial pH. In: RJ Gilkes and N Prakongkep (eds). 19th World Congress of Soil Science, Soil Solutions for a Changing World, 1 – 6 August 2010, Brisbane, Australia,  pp. 160-163.Syahrawat KL.  2006.  Organic matter and mineralizable nitrogen relationships in wetland rice soils.  Commun Soil Sci Plant Anal 37: 787-796. Wagai R and LM Mayer.  2007.  Sorptive stabilization of organik matter in soils by hydrous iron oxides.  Geochim Cosmochim Act 71: 25-35.Watanabe I.  1984.  Anaerobic decomposition of organic matter in flooded rice soils. In: Organic Matter and Rice. Intenational Rice Research Institute.  Los Banos Laguna, Philippines,  pp. 237-258.Wickham TH and VP Singh. 1978.  Water movement through wet soils. Soil and Rice.  International Rice Research Institute. Los Baños, Philippines, pp. 337- 358.
Influence of Height Waterlogging on Soil Physical Properties of Potential and Actual Acid Sulphate Soils Fahmi, Arifin; Susilawati, Ani; Rachman, Ahmad
JOURNAL OF TROPICAL SOILS Vol. 19 No. 2: May 2014
Publisher : UNIVERSITY OF LAMPUNG

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.5400/jts.2014.v19i2.67-73

Abstract

Water management is main factor that determines the successful of rice cultivation in acid sulphate soil. Soil waterlogging determines the direction and rate of chemical, geochemical and biological reaction in the soil, indirectly these reactions may influence to the changes of soil psycal properties during soil waterlogging process. The experiment was aimed to study the changes of two type of acid sulphate soils physical properties during rice straw decomposition processes.  The  research  was  conducted  in  the  greenhouse  consisting  of  the  three  treatment  factors  using  the completely randomized design with three replications. The first factor was soil type: potential acid sulphate soil (PASS) and actual acid sulphate soil (AASS). The second factor was height of water waterlogging: 0.5-1.0 cm (muddy water–level  condition) and 4.0 cm from above the soil surface (waterlogged). The third factor was organic matter type: rice straw (RS), purun tikus (Eleocharis dulcis) (PT) and mixed of RS and PT (MX). Soil physical properties such as aggregate stability, total soil porosity, soil permeability, soil particle density and bulk density were observed at the end of experiment (vegetative maximum stage). The results showed that acid sulphate soil type had large effect on soil physicl properties, soil waterlogging decreased aggregate stability, soil particle density and bulk density both of soil type.Keywords : Acid sulphate soils, soil physical properties, and waterlogging [How to Cite: Arifin F, A Susilawati and A Rachman. 2014. Influence of Height Waterlogging on Soil Physical Properties of Potential and Actual Acid Sulphate Soils. J Trop Soils 19(2): 77-83. Doi: 10.5400/jts.2014.19.2.77]
Co-Authors Andree Saylendra, Andree Andrie Kurniawan Anna Hairani ARIFIN FAHMI Aziz Mustofa Anwar, Abdul Bin Has, Qois Azizah Dedi Nursyamsi Dedi Wahyudi Dewi, Lusiana Puspa Eka Priyantoro, Dian Eni Maftu’ah Erwin Erwin Faroman Syarief Faroman Syarief, Faroman Firdaus, Rizki Amsyarul Haris Syahbuddin Herviana, Ditta Ahmad Izhar Khairullah Jarinah, Jarinah Kartini, Tini Khotijah Khotijah Linda Indrayati Lutfi Izhar Maman Suherman MUHAMMAD ALI Mulyaningsih, Asih Munawaroh Nurhakiki, M. Nurkholis Nurkholis Nurul Anriani Putri, Widiya Rachman, Ahmad Saripudin, Yusep Sartika, Nenden Suciyati Suhardoyo Suharyanto H. Soro Sustama, Achmad Adi Surya Tarso Rudiana, Tarso Tuti Rostianti Maulani Ucu Wandi Somantri Wiyono, Slamet Yani, Achmad