Pengaruh Pasang Surut terhadap Pengendapan Lumpur di Lahan Sawah Rawa Kawasan Sungai Barito Kalimantan Selatan

https://doi.org/10.22146/agritech.33863

M Mawardi(1*), Putu Sudira(2), Bambang Hendro Sunarminto(3), Totok Gunawan(4), Benito Hadi Purwanto(5)

(1) Departemen Ilmu Tanah, Fakultas Pertanian, Universitas Gadjah Mada, Jl. Flora, Bulaksumur, Yogyakarta 55281
(2) Departemen Teknik Pertanian dan Biosistem, Fakultas Teknologi Pertanian, Universitas Gadjah Mada, Jl. Flora No. 1, Bulaksumur, Yogyakarta 55281
(3) Departemen Ilmu Tanah, Fakultas Pertanian, Universitas Gadjah Mada, Jl. Flora, Bulaksumur, Yogyakarta 55281
(4) Fakultas Geografi, Universitas Gadjah Mada, Jl. Kaliurang, Sekip Utara, Bulaksumur, Yogyakarta 55281
(5) Departemen Ilmu Tanah, Fakultas Pertanian, Universitas Gadjah Mada, Jl. Flora, Bulaksumur, Yogyakarta 55281
(*) Corresponding Author

Abstract


Swamp land has a great potential to be developed as a paddy field area. However it has many constraints such as-phyrite (FeS2) at the depth of 30–60 cm and lack of soil nutrition. On the other hand, supply of marine clay from the sea which contains a lot of smektit clay mineral can be used to netralize this condition. Mud clay is very important for the development of rice root because it contains much nutrition and to enlarge the top of soil reducing the oxidation of phyrite. This study was conducted from January 2016 to June 2017 in swamp land area of Barito River of South Kalimantan. Data was collected by measuring the difference between maximum and minimum sea tide (tidal amplitude) and the deposition of mud clay. The results indicated that the distribution of mud clay deposit vary depends on the geography and the tidal amplitude of the zone. Zone VII has higher concenration of mud clay than the other one. The distribution pattern of mud clay deposit follows the parabola type, verticaly and horizontaly type, as well. Increasing of mud clay at all of the zone areas are not significantly effected by the daily tidal amplitude, only depends on climate condition/the season change.

Keywords


Mud clay; phyrite; tidal of the sea; tidal rice field

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References

BPS, 2017. Kabupaten Barito Kuala. Produksi Padi Sawah Menurut Kecamatan di Kabupaten Barito Kuala, 2011- 20015. (https://baritokualakab.bps.go.id/dynamictable/2017/01/17 /864/produksi-padi-sawah-menurut-kecamatan-di-kabupaten-barito-kuala-2011-2015.html).

Franco, A. D. S., 1966, Tides.Fundamentals, prediction and analysis, International Hydrographic Office, Monaco.

Hariyanto, T., Krisna, T. C., & Pribadi, C. B. (2017). Development of Total Suspended Sediment Model using Landsat-8 OLI and In-situ Data at the Surabaya Coast , East Java, Indonesia, 49(1), 73–79.

Hydrographer of the Nurry 1969, Tides and tidal streams, Admiralty of Hydrographic Surveyimg, Taunton. Hydrographer of the Nurry, 1969, Tides and tidal streams, Admiralty of Hydrographic Surveyimg, Taunton.

Hydrographic Hydrographic Services, 1987, Physical oceanographic survey course, Group Training Course In Hydrographic Services, Tokyo.

Klasifikasi, M. D. A. N., Hardjowigeno, S., Subagyo, H., & Rayes, M. L. (1950). 1. morfologi dan klasifikasi tanah sawah, 1–28.

Mahmud, Joko H. Susanto. (2009). Penilaian Status Daerah Aliran Sungai ( Studi Kasus Sub Das Serang ), Journal AGRITECH, Vol. 29, No. 4 November 2009

Marchuk, G. L, Kagan, B. A., 1983, Dynamics of ocean tides, Kluwer Academic Publizshers, Dordrecht.

Noor, M. 2004. Lahan Rawa Sifat dan Pengelolaan Tanah Bermasalah Sulfat Masam. Divis Buku Perguruan Tinggi. Raja Grafindo Persada. Jakarta.

Pariwono, J., 1985, Australian cooperative programmes in marine sciences: tides and tidal phenontena in the ASEAN region, Fl inders University, Flinders).

Shamsuddin, J., S. Muhrizal, I, Fauziah and E Van Ranst. 2004. A.laboratory study of pyrite oxidation in acid sulfate solils. Communication in Soil Science and Plant Analysis.

Subagyo, H. 2006. Karakteristik dan Pemgelolaan Lahan Rawa. Lahan Rawa Pasang Surut. Balai Besar Penelitian dan Pengembangan Sumberdaya Lahan Pertanian. Badan Penelitian dan Pengembangan Pertanian. Departemen Pertanian. Jakarta. ISBN 979-9474-52-3

Sudana, W. (2005). Potensi dan prospek lahan rawa sebagai sumber produksi pertanian. Analisis Kebijakan Pertanian, 3, 141–151.

Suriadikarta, uriadikarta, D. A. (2012). Teknologi Pengelolaan Lahan Rawa Berkelanjutan : Studi kasus Kawasan EX PLG Kalimantan Tengah. (Technology for Sustainable Management of Tidal Swampy Areas: Case Study in former PLG in Central Kalimantan Povince) Journal Sumberdaya Lahan Vol. 6 No. 1, Juli 2012.

Thuy, N. N., & Anh, H. H. (2015). Vulnerability of Rice Production in Mekong River Delta under Impacts from Floods , Salinity and Climate Change, 5(4), 272–279.

Try Al Tanto, Ulung Jantama Wisha, Gunardi Kusumah, Widodo S Pranowo, Semeidi Husrin, & Aprizon Putra. (2017). Characteristics of Sea Current in Benoa Bay Waters – Bali. Ilmiah Geomatika, 23(1), 37–48. https://doi.org/10.24895/JIG.2017.23-1.%25x

Unesco, 1994. Manual on sea level measurement and interpretation. Volume l-Basic procedures, Intergovermental Oceanographic Commission, Paris.



DOI: https://doi.org/10.22146/agritech.33863

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