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Reclamation of Ex-Mining Land for Agricultural Extensification DARIAH, AI; ABDURACHMAN, A.; SUBARDJA, DJADJA
Jurnal Sumberdaya Lahan Vol 4, No 01 (2010): Juli 2010
Publisher : Indonesian Center for Agriculture Land Resource Development

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Utilization of ex-mining land for agricultural extensification is an opportunity to solve the problem of food and environment. This paper discusses prospective utilization of ex-mining land for agricultural extensification. Mining area equipped with a business license for mining in Indonesia is around 2.2 million ha under Coal Concession Agreement, and 2.9 million ha under the Contract of Effort. A part of land is already finished being mined, and be managed properly in order to benefit the community and not damage the environment. The initial steps that need to be done is mapping of mined lands, included a status of ownership (land tenure), so that subsequent use of both for agriculture and other businesses can be sustainable. Land reclamation is necessary to increase capacity and efficiency for biomass production. Determination of land use types, should be based on land tenure, bio-physical conditions of land, and the needs of the community or local government. In the future, mining land management requirements is not enough simply by opening a feasibility study for mining operations, but need to be accompanied also with itsclosure plan (planning of closures), which includes environmental protection and mitigation of socio-economic problems. This needs to be one of the terms of the granting of mining permits.

PENGARUH TINGGI MUKA AIR SALURAN DRAINASE, PUPUK, DAN AMELIORAN TERHADAP EMISI CO 2 PADA PERKEBUNAN KELAPA SAWIT DI LAHAN GAMBUT DARIAH, AI; JUBAEDAH, JUBAEDAH; WAHYUNTO, WAHYUNTO; PITONO, JOKO
853-8212
Publisher : Pusat Penelitian dan Pengembangan Perkebunan

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ABSTRAKDrainase yang berlebihan dan penggunaan pupuk yang intensifdiduga menjadi penyebab tingginya emisi gas rumah kaca (GRK) padaperkebunan kelapa sawit di lahan gambut. Penelitian ini bertujuan untukmempelajari pengaruh tinggi muka air (TMA) saluran drainase, pupuk,serta amelioran terhadap emisi CO 2Â dari perkebunan kelapa sawit di lahangambut. Penelitian dilakukan dari bulan Januari 2010 sampai denganDesember 2011, pada perkebunan sawit di lahan gambut, di KecamatanSiak Kecil, Kabupaten Bengkalis, Riau, menggunakan rancangan petakterpisah, tiga ulangan. Petak utama adalah TMA saluran drainase (40, 60,dan 80 cm). Anak petak adalah pupuk dan amelioran: (1) dolomit 3kg/pohon/tahun; (2) Pugam 10 kg/pohon/tahun; (3) Pupuk dosisrekomendasi (2,5 kg urea+2,75 kg SP-36+2,25 kg KCl+dolomit 2kg)/pohon/tahun; (4) Pupuk 75% dosis rekomendasi pukan 20kg/pohon/tahun; (5) Pupuk 75% dosis rekomendasi Pugam 2,5 kg/pohon.Parameter yang diamati adalah fluks CO 2 . Hasil penelitian menunjukkanbahwa pada TMA drainase 80 cm, perlakuan dolomit menghasilkan fluksCO 2 nyata paling tinggi (142,1 t/ha/tahun) dan terendah (44,5 t/ha/tahun)dicapai perlakuan pugam. Fluks CO 2 yang tinggi (130,6 t/ha/tahun) jugadicapai perlakuan pupuk dosis rekomendasi, khususnya pada TMA 40 cm.Pada musim kemarau TMA drainase berpengaruh nyata terhadap fluksCO 2 , terendah dicapai TMA 40 cm. Oleh karena itu, untuk meminimalkanemisi gas CO 2 , maka TMA drainase perlu dipertahankan sedangkalmungkin (sekitar 40 cm) selama tidak menurunkan produksi kelapa sawit.Amelioran dengan bahan aktif kation polyvalen berpotensi dapat menekanemisi GRK dari lahan gambut yang dikelola secara intensif.Kata kunci: amelioran, emisi, drainase, gambut, kelapa sawit, pupukABSTRACTExcessive drainage and intensive use of fertilizers thought to bethe cause of high greenhouse gas emissions in peatland under oil palmplantations. The study aimed at measuring the influence of water leveldrainage (WLD), fertilizer, and ameliorant on CO 2 emissions from oilpalm plantations on peatland. The study was conducted from January2010 to December 2011, at oil palm plantation on peatland, located in SiakKecil District, Bengkalis Regency, Riau, using split plot design, with threereplications. The main plot were WLD (40, 60, and 80 cm), as sub plotswere fertilizer and amelioran: (1) dolomite 3 kg/tree/year; (2) peatfertilizer 10 kg/tree/year; (3) dose of fertilizer recommendations (2,5 kgurea+2,75 kg SP-36+2,25 kg KCl+dolomite 2 kg)/tree/year; (4) 75% doseof fertilizer recommendations + manure 20 kg/tree/year; (5) 75% dose offertilizer recommendations + peat fertilizer 2.5 kg/tree/year. Parameterobserved was CO 2 flux. The result showed that at WLD 80 cm, dolomitetreatment resulted the highest (142,1 t/ha/year) and the lowest CO 2Â flux(44,5 t/ha/year) resulted by peat fertilizer. The highest CO 2 flux alsoreached by fertilizer recommendations treatment, particularly on WLD 40cm. In dry season WLD significantly effect on CO 2 flux. The lowestreached by WLD 40 cm. Based on that the WLD needs to be maintainedin a state of shallow (approximately 40 cm), without lowering production.The use of fertilizer containing ameliorant with the polyvalen cation asactive material, potentially suppress the rate of greenhouse gas emissionsfrom peatlands are managed intensively.Key words: ameliorant, emission, drainage, peatland, oil palm, , fertilizer

THE USE OF MINERAL AND ORGANIC SOIL CONDITIONER TO IMPROVE SOIL QUALITY OF TYPIC KANHAPLUDULTS TAMANBOGO, LAMPUNG DARIAH, AI; SUTONO, .; NURIDA, NENENG LAILA
Jurnal Tanah dan Iklim (Indonesian Soil and Climate Journal) No 31 (2010): Juli 2010
Publisher : Balai Besar Penelitian dan Pengembangan Sumberdaya Lahan Pertanian

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.21082/jti.v0n31.2010.%p

As soil conditioner, there are many functions of organic matter that would not be replaced by mineral material. Therefore, mineral soil conditioner is better focused on increasing quality of organic soil conditioner. The objective of the research was to obtain the effectiveness of soil conditioner formula (organic matter and zeolit) and its application technique (dose and phase application) in improving soil quality. The research was conducted at KP Tamanbogo, Lampung for three seasons (2006/2007). The experiment employed a split plot design with three reflications. Application techniques of soil conditioner (dose and phase aplication) as main plots and three types formula of soil conditioner as sub plots. Corn was used as test crop. Parameters observed were plant growth and production, and changes in soil properties. The results showed that soil conditioner that applied on Typic kanhapludults could significantly increased corn growth and yield. Soil conditioner with higher organic matter proportion has better effect on corn growth and yield as well as on physical soil properties, which indicated by soil permeability and aggregate stability. The addition of 20% of zeolit in soil conditioner formula increased soil microorganism activities, but the additional up to 30% decrease microorganism activities. The changes of organic matter and zeolit proportion in soil conditioner has significantly effect on soil pH and N content, but has no significantly effect on P, K content, and CEC. Compared to innitial soil condition, application of soil conditioner could increase CEC from <4 cmolc kg-1 to 5.85 cmolc kg-1 respectively. Soil conditioner was better to be applied periodically but must be done every season. For degraded soil such as at KP. Tamanbogo, soil conditioner was applied with 10 t ha-1 dose for innitial rehabilitation process, hereinafter with 5 t ha-1 annual crop season dose.

RELATIONSHIP BETWEEN SOIL CHARACTERISTICS AND RATE OF SOIL LOSS ON COFFEE BASE-FARMING SYSTEM AT SUMBERJAYA, WEST LAMPUNG DARIAH, AI; AGUS, F.; ARSYAD, S.; SUDARSONO, .; MASWAR, .
Jurnal Tanah dan Iklim (Indonesian Soil and Climate Journal) No 21 (2003): Desember 2003
Publisher : Balai Besar Penelitian dan Pengembangan Sumberdaya Lahan Pertanian

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.21082/jti.v0n21.2003.%p

The current public perception concerning land use change is, whenever forest is converted to agricultural land, the forest functions would drasticaly decrease. Studies have shown that soil loss in coffee based systems varied widely and it could be much lower than the tolerable soil loss level, depending on soil properties. This research was conducted to determine the dominant factors of soil properties in influencing soil loss. This analysis was based on data collected from a 3-site (Laksana, Tepus and Bodong Sub-Village of Sumberjaya Village, West Lampung) erosion study in 2001/2002. Observation of soil properties for each site was carried out by soil profile description and quantitative laboratory analyses for several soil physical properties and organic C content. Samples were collected from three soil depths namely 0-10, 10-20 and 20-40 cm. The resultsindicated that soil physical properties were dominant factors determining soil loss level in coffee-based farming system in Sumberjaya. The erosion on soil with mean total porosity of > 65%, macro pore of > 24%, and soil permeability of > 9 cm hr-1 was < 2 t ha-1 yr-1. Whereas erosion of soil with porosity of < 60%, macro pore of < 13%, and soil permeability of < 3 cm hr-1 was 37 t ha-1 for 3 months. These results suggested that soilconservation recommendation, particularly for Sumberjaya coffeebasedsystems, should not be imposed uniformly across sites. Site-specific soil property characterization and hence evaluation of soil susceptibility to erosion should precede recommendation and implementation emphasized only on erosion-prone sites.

How Do Groundwater Levels and Soil Moisture Influence the Peat Fire Vulnerability Index in Oil Palm Plantations? Purnamayani, Rima; Tarigan , Suria Darma; Sudradjat, Sudradjat; Syahbuddin, Haris; Dariah, Ai; Kartiwa, Budi
Journal of Tropical Crop Science Vol. 12 No. 01 (2025): Journal of Tropical Crop Science
Publisher : Department of Agronomy and Horticulture, IPB University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29244/jtcs.12.01.235-245

Peatland fires are a significant environmental issue, impacting local ecosystems and contributing to global climate change. This study evaluates the Peat Fire Vulnerability Index (PFVI) for sapric and hemic maturity levels under oil palm plantations in Pangkalan Pisang Village, Riau Province. Data on groundwater level, soil moisture, rainfall, and maximum temperature were collected from December 2021 to December 2022. The PFVI, modified from the Keetch-Byram Drought Index (KBDI), was calculated and correlated with these variables. The groundwater level varied from 3 cm to 76 cm below the surface, with an average of 36.23 cm. In sapric blocks, 29% of the groundwater level was less than 40 cm, while 73% were deeper. In hemic blocks, 44% were less than 40 cm, and 56% were deeper. Soil moisture in the top 10 cm layer fluctuated between 32% and 55% (v/v) Results showed significant negative correlations between PFVI and groundwater levels (r = -0.173 to -0.889) and soil moisture (r = -0.835 to -0.808), indicating that lower groundwater levels and soil moisture increase fire risk. High PFVI values in July corresponded with the lowest rainfall (59 mm) and groundwater levels below 40 cm. The study highlights the importance of monitoring hydrometeorological conditions and soil properties to effectively predict and mitigate peatland fires. Our findings are crucial for developing strategies to manage peatland sustainability and reduce fire hazards, especially in tropical regions with prevalent oil palm cultivation.

Spatial distribution of water quality in water bodies influenced by agricultural activities Yustika, Rahmah Dewi; Sukarjo, Sukarjo; Dewi, Triyani; Yustiawati, Yustiawati; Handayani, Cicik Oktasari; Yanti, Delvi; Dariah, Ai
Journal of Degraded and Mining Lands Management Vol. 12 No. 4 (2025)
Publisher : Brawijaya University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.15243/jdmlm.2025.124.8367

Agriculture is a major contributor to non-point source pollution due to the intensive use of agrochemicals. This study examined the spatial distribution of pollutants from agricultural activities in the Sumani sub-catchment, West Sumatra, Indonesia, which drains into Lake Singkarak. Thirteen water quality parameters were measured, including electrical conductivity (EC), total suspended solids (TSS), total dissolved solids (TDS), dissolved oxygen (DO), sulfate, nitrate, calcium, sodium, total phosphorus (TP), potassium, magnesium, chlorpyrifos, and mancozeb. Results showed significant variation in water quality across the sampling sites. Downstream areas had higher levels of TSS, TDS, and major ions, mainly due to agricultural and urban activities. The lowest TSS levels were recorded at a site within the lake, likely due to sediment settling. River water generally met drinking water standards; however, TP and DO concentrations in the lake exceeded regulatory limits, potentially influenced by floating net cage aquaculture. Principal Component Analysis identified three main sources of pollution: agricultural activities (34.87%), combined agricultural and urban influences (20.15%), and soil erosion (12.15%). These findings highlight the need for better erosion control, sustainable farming practices, and consistent water quality monitoring. Further research is crucial to understand the long-term effects of agriculture on water resources and to develop strategies that reduce environmental impacts.

Relationship between Distance Sampling and Carbon Dioxide Emission under Oil Palm Plantation Dariah, Ai; Agus, Fahmuddin; Susanti, Erni; Jubaedah, .
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.v18i2.125-130

Carbon dioxide emission on peatland under oil palm plantation were highly varied probably due to many factors involved. The objectives of the research were to evaluate the effect of distance sampling from center of oil palm tree on Carbon dioxide flux, and to study the factors that cause variability of carbon dioxide flux on peatland under oil palm plantation. The study was conducted on peatland at Arang-Arang Village, Kumpek Ulu Sub-District, Muaro Jambi District, Jambi Province, on six year old oil palm plantation. The study was conducted in the form of observational exploratory. Emission measurements performed on 5 selected oil palm trees at points within 100, 150, 200, 250, 300, 350, and 400 cm from the center of trunk. Carbon dioxide flux was measured using (IRGA), Li-COR 820. The results showed that there is significant correlation between the distance of sampling from center of oil palm tree and Carbon dioxide flux. The farther distance from the tree, Carbon dioxide flux more decreased. Before applying fertilizer, variability of soil fertility was not significantly correlated with the flux of Carbon dioxide, so the difference of Carbon dioxide flux based on distance sampling can be caused by root distribution factor. After fertilizer application, variability of Carbon dioxide flux under the oil palm tree were beside affected by differences in root distribution, was also greatly influenced by fertilization.Keywords: Carbon dioxide flux, distance sampling, oil palm, peat, root-related respiration [How to Cite: Dariah A, F Agus, E Susanti and Jubaedah. 2013.Relationship between Sampling Distance and Carbon Dioxide Emission under Oil Palm Plantation. J Trop Soils 18 (2): 125-130. Doi: 10.5400/jts.2013.18.2.125][Permalink/DOI: www.dx.doi.org/10.5400/jts.2013.18.2.125] REFERENCESAgus F, E Handayani, van M Noordwijk, K Idris and S Sabiham. 2010 Root respiration interferes with peat CO2 emission measurement. 19th World Congress of Soil Science, Soil Solutions for a Changing World. 1 - 6 August 2010, Brisbane, Australia. Published on DVD.Amador JA and RD Jones. 1993. Nutrient limitation on microbial respiration in peat soil with diffrent total phosphorus content. Soil Biol Biochem 25: 793-801.Franklin O, P Hoogberg, A Ekbled and GI Agren. 2003. Pine forest floor carbon accumulation in response to N and PK addition: Bomb C-14 modeling and respiration studies. Ecosystem 6: 644-658. Freeman C, N Ostle and H Kang. 2001. An Enzymic ‘latch’ on global carbon store-a shortage of oxigen locks up carbon in peatlands by restraining a single enzyme. Nature 409: 149-149.Hanson PJ, NT Edwards, CT Garten and JA Andrew. 2000. Separating root and soil microbial contributions to soil respiration: A review of methods and observations. Biogeochemistry 48: 115-146.Henson IE, and SH Chai. 1997. Analysis of oil palm productivity. II. Biomass, distribution, productivity and turnover of the root system. Elaeis 9: 78-92.Hergoualc’h K and LV Verchot. 2011. Stocks and fluxes of carbon associated with land use change in Southeast Asian tropical peatlands: A review. Glob Biogeochem Cycl 25. doi:10.1029/2009GB003718.Howarth RW and SG Fisher. 1976. Carbon, nitrogen, phosporus dynamic during leaf decay in nutrient-enriched stream microecosystems. Freshwater Biol 6: 221-228.Husen E and F Agus. 2011. Microbial activities as affected by peat dryness ans ameliorant. Am J Environ Sci 7: 348-353.Jauhiainen J, A Hooijer and SE Page. 2012. Carbon dioxide emissions from an Acacia plantation on peatland in Sumatra, Indonesia. Biogeosciences 9: 617–630. DOI:10.5194/bg-9-617-2012.Khalid H, ZZ Zin and JM Anderson. 1999. Quantification of oil palm biomass and nutrient value in mature planttation. II Below-ground biomass. J Oil Palm Res 11: 63-71.Knorr KH, MR Oosterwoud and C Blodau. 2008. Experimental drought alters rates of soil respiration and methanogenesis but not carbon exchange in soil of a temperate fen. Soil Biol Biochem 40: 1781-1791.Law BE, FM Kelliher, DD Baldocchi, PM Anthoni, J. Irvine, D. Moore and SV Tuyl. 2001. Spatial and temporal variation in respiration in a young ponderosa pine forest during a summer drought. Agric Forest Meteorol 110: 27-43.Laiho R, J Laine, CC Trettin and L Finner. 2004. Scot pine litter decomposition along drainage succession and soil nutrient gradient in peat land forest, and the effect of inter-annual weather variation. Soil Biol Biochem 36: 1095-1109.Madsen R, L Xu, B Claassen and D McDermit. 2009. Surface monitoring method for carbon capture and storage projects. Energy Procedia 1: 2161-2168Martoyo K. 1992. Kajian Sifat Fisik Tanah Podsolik untuk Tanaman Kelapa Sawit (Elaeis gueneensis Jacq) di Sumatera Utara. Tesis Program Pasca Sarjana, Universitas Gajah Mada. Yogyakarta (in Indonesian).Melling L, R Hatano and KJ Goh. 2007. Nitrous oxide emissions from three ecosystem in tropical peatlands of Sarawak, Malaysia. Soil Sci Plant Nutr 53: 792-805.Minkkinen K, J Laine, NJ Shurpali, P Makiranta, J Alm and T Pentilla. 2007. Heterotropic soil respiration in forestry-drained peatland. Boreal Environ Res 12: 115-126. Murdiyarso D, K Hergoualc’h K and LV Verchot. 2010 Opportunities for reducing greenhouse gas emissions in tropical peatlands. PNAS 107: 19655-19660.Olsen R, S Linden, R Giesler, and P Hogberg. 2005. Fertilization of boreal forest reduce of both autrotrophic dan heterotrophic soil respiration . Glob Change Biol 11: 1745-1753.Silvola J, J Valijoki and H Aaltonen. 1985. Effect of draining and fertilization on soil respiration at three ameliorated peatland site. Acta For Fem 191: 1-32.Silvola J, J Alm, U Aklholm, H Nykanen and PJ Martikainen. 1996a. Carbon dioxide fluxes from peat in boreal mires under varying temperature and moisture condition. J Ecol 84: 219-228.Silvola J, J Alm, U. Ahlholm, H Nykanen, and PJ Martikainen. 1996b. The contribution of plant roots to carbon dioxide fluxes from organic soils. Biol Fertil Soils 23: 126-131.Wang W, K Ohseb and J Liuc. 2005. Contribution of root respiration to soil respiration in a C3/C4 mixed grassland. J Bioscience 30: 507-514.

Relationship between Sampling Distance and Carbon Dioxide Emission under Oil Palm Plantation Dariah, Ai
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.%p

A carbon dioxide emission on peatland under oil palm plantation was highly varied due to many factors involved. The objectives of the research were to evaluate the effect of sampling distance from center of oil palm tree on Carbon dioxide flux, and to study the factors that cause variability of carbon dioxide flux on peatland under oil palm plantation. The study was conducted on peatland at Arang-Arang Village, Kumpek Ulu Sub-District, Muaro Jambi District, Jambi Province, on six-years old oil palm plantation. The study was conducted in the form of observationalexploratory. Emission measurements were performed on 5 selected oil palm trees at points within 100, 150, 200, 250,300, 350, and 400 cm from the center of trunk. Carbon dioxide flux was measured using (IRGA), Li-COR 820. The results showed that there was significant correlation between the distance of sampling from center of oil palm tree and Carbon dioxide flux. The farther distance from the tree, the more decreased of Carbon dioxide flux . Before applying fertilizer, variability of soil fertility was not significantly correlated with the flux of Carbon dioxide, so the difference of Carbon dioxide flux based on distance sampling can be caused by root distribution factor. After fertilizer application, variability of Carbon dioxide flux under the oil palm tree were not only affected by differences in root distribution but also greatly influenced by fertilization.Keywords: Carbon dioxide flux, distance sampling, oil palm, peat, root-related respiration

The Effectiveness of Ameliorant to Increase Carbon Stock of Oilpalm and Rubber Plantation on Peatland Dariah, Ai
JOURNAL OF TROPICAL SOILS Vol. 20 No. 2: May 2015
Publisher : UNIVERSITY OF LAMPUNG

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.5400/jts.2015.v20i2.67-75

Application of peatland amelioration can improve soil quality, reduce GHG emissions, and increase carbon sequestration. The research aimed to study the effect of peatland amelioration on oil palm and rubber carbon stock improvement. Research was conducted from August 2013 until June 2014. The researches on oil palm were done in Arang-arang Village, Kumpeh Subdistrict, Muaro Jambi District, and in Lubuk Ogong Village, Bandar Seikijang Sub-district, Pelalawan District. Both sites are in Jambi and Riau Province. The research on rubber was done in Jabiren Village, Jabiren Raya Subdistrict, Pulang Pisau District, Central Kalimantan Province. The study used a Randomized Completely Block Design (RCBD), in four treatments and four replications. The treatments were pugam (peat fertilizer enriched by polyvalent cation), manure; empty fruit bunch compost, and control (no application). The measurement of C stock was performed 10 months after application using nondestructive methods. The results showed that peatland amelioration treatments had no significant effect to improve C stock on oil palm in 6 years old and 7 years old of rubber. After 10 months of amelioration application, the treatments increased C - stock of oil palm and rubber were 2.1-2.4 Mg ha-1 and 5-11 Mg ha-1, respectively. Longer time observation may be needed to study the effect of ameliorant on C-stock of annual crops.

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