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The Effects of Organic Matter and N, P, K Fertilizer on Nutrient Uptake and Yield of Corn in Inceptisol Ternate Idris Abd Rachman; Sri Djuniwati; Komarudin Idris
Jurnal Ilmu Tanah dan Lingkungan Vol 10 No 1 (2008): Jurnal Ilmu Tanah dan Lingkungan
Publisher : Departemen Ilmu Tanah dan Sumberdaya Lahan, Fakultas Pertanian, IPB University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (520.157 KB) | DOI: 10.29244/jitl.10.1.7-13

Abstract

The objective oj the research was to study the effects oj organic matter and N, P, K Jertilizer on nutrients uptake andyield oj corn in Inceptisol Ternate. The design oj the research was Jactorial completely randomized block design with twoJactors. The first Jactor was the rate oj organic matter (0, 20, 40 tlha) or (B(), B, and B z) and the second Jactor was the rate oj N, P, KJertilizer (0.5; I and /.5 recommended rate) or (Flo F] and F JJ. The results oj research showed that combination oj B ,F] gave the highest amount oj the corn leave at 42 days afterplanting, the weight oj corn with husk cover, the weight corn grains, and K-availability oj soil. Whereas, the rate oj 20 tlhaorganic matter (B,) significantly increased and gave the highest weight oj corn without husk cover, NPK corn plant contentand P uptake. The average NPK plant uptake oJcorn was 31.41-39.39 kg Nlha, 6.03-/2.54 kg Plha, 37.5-41.70 kg Klha. The average production oj corn was 5. /6-7.83 tlha.
PEMBERIAN KOTORAN SAPI PADA PERTANAMAN JAGUNG (Zea mays): PERUBAHAN FRAKSI FOSFOR INORGANIK PADA ULTISOL GUNUNG SINDUR, JAWA BARAT Arief Hartono; Sri Djuniwati; Hafiz Hernandi
Jurnal Ilmu Tanah dan Lingkungan Vol 15 No 1 (2013): Jurnal Tanah dan Lingkungan
Publisher : Departemen Ilmu Tanah dan Sumberdaya Lahan, Fakultas Pertanian, IPB University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (286.608 KB) | DOI: 10.29244/jitl.15.1.1-4

Abstract

Percobaan mengenai evaluasi perubahan fraksi-fraksi fosfor (P) karena pemberian kotoran sapi pada budidaya jagung dilaksanakan di desa Cibadung Gunung Sindur, Jawa Barat. Dosis kotoran sapi yang digunakan adalah 0, 10, 20, dan 40 ton ha-1. Percobaan dilakukan menggunakan rancangan acak lengkap dengan tiga ulangan. Pengambilan contoh tanah dilakukan setelah dua minggu inkubasi dan setelah panen. Contoh tanah diambil di rhizosfer dan antar baris tanaman. Perubahan fraksi-fraksi P dievaluasi dari hasil pengurangan nilai suatu fraksi P pada saat panen dengan nilai suatu fraksi P setelah dua minggu inkubasi. Hasil menunjukkan bahwa pemberian kotoran sapi nyata meningkatkan fraksi resin-Pi, fraksi NaHCO3-Pi dan NaOH-Pi. Nilai fraksi-fraksi P tersebut pada saat panen lebih tinggi di rhizosfer dibandingkan dengan nilai fraksi-fraksi P di antar baris tanaman. Perubahan resin-Pi di rhizosfer dan antar baris tanaman adalah negatif yang menunjukkan bahwa resin-Pi telah bertransformasi ke fraksi P yang lain. Perubahan fraksi NaHCO3-Pi dan NaOH-Pi tidak konsisten positif baik di rhizosfer dan antar baris tanaman dengan meningkatnya dosis kotoran sapi. Hal ini menunjukkan bahwa pengambilan P oleh tanaman, pelepasan P dan transformasi P ke bentuk yang lebih stabil mempengaruhi jumlah peningkatan fraksi NaHCO3-Pi dan NaOH-Pi.
THE STATUS OF SOIL PHOSPHORUS AT DIFFERENT CROPPING SYSTEM IN PANGALENGAN, SOUTH BANDUNG Sri Djuniwati; Heru Bagus Pulunggono
Jurnal Ilmu Tanah dan Lingkungan Vol 11 No 2 (2009): Jurnal Ilmu Tanah dan Lingkungan
Publisher : Departemen Ilmu Tanah dan Sumberdaya Lahan, Fakultas Pertanian, IPB University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (280.23 KB) | DOI: 10.29244/jitl.11.2.76-80

Abstract

The fixation of P in soils is dynamic in nature and the behavior of P-fraction may change with time and cropping system. Application of organic matter to soil under upland soil have been reported to decrease P-sorption and increase P-desorpion.  Pangalengan, South Bandung in west Java is one of the wet humid area of Indonesia that has high rain fall, covered mainly by tropical humid forest, volcanic area with fertile volcanic soil. The objective of this study were to describe and compare some chemical characteristic and behavior of P-fraction as a function of  crops and slope of the land in the farming system in Pangalengan, South Bandung, West Java, Indonesia. Soil samples from the surface soil (0-20 cm) were collected from 15 locations based on different planted crops (Tea, Vegetables, Forest, and Intercropping crops),  and level of slope of the land areas of Cihawuk village, District Kertasari, Kecamatan Pangalengan.  The result of the study showed that C-organic content of  soil samples from 15 location of planted crops was slightly high (3.04-4.92 %) but total Nitrogen was low (0.22-0.45 %), wih soil reaction (pH H2O) was  slightly acids (5.60-6.30) and pH (KCl) was lower than pH(H2O) (4.60-5.70).    The  available-P was low (3.50 – 7.10 ppm), but the HCl 25 % P from  tea and vegetables  location was higher than from forest and intercropping crops.   Majority of P fraction  from tea and vegetable location was Al-P fraction, but from Forest and intercropping crops was  Ca-P fraction. The order of P fraction were Al-P > Ca-P> reductant soluble-P>Fe-P in tea and vegetables locations, but in the forest and intercropping were Ca-P> reductant-P > Al-P > Fe-P.  However, The data showed that the total P (P-organic + P-inorganic) from tea and vegetables crop location was higher, and was dominated by inorganic form, than from forest and intercropping location was dominated by organic form.  However, the slope did not affect the pattern of P-fractions and   the sources of organic matter added or accumulated in those location formerly  affected the amount and the pattern of P-fractions.
The Effects of Various Water Table Depths on CO2 Emission at Oil Palm Plantation on West Aceh Peat Handayani, Etik Puji; Noordwijk, Meine Van; Idris, Kamarudin; Sabiham, Supiandi; Djuniwati, Sri
JOURNAL OF TROPICAL SOILS Vol. 15 No. 3: September 2010
Publisher : UNIVERSITY OF LAMPUNG

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.5400/jts.2010.v15i3.255-260

Abstract

The Effects of Various Water Table Depths on CO2 Emission at Oil Palm Plantation on West Aceh Peat (EP  Handayani, M van Noordwijk, K Idris,  S Sabiham and S Djuniwati):  Changes in the depth of water table influenced carbon cycling in peatlands, and affected the sources and sinks of carbon dioxide.  The effects of depth of water tables in oil palm plantations on the emission of CO2 were studied. CO2 emissions of peatland were measured in Meulaboh, West Aceh using cylindrical chambers and  air samples from the chambers were analyzed by gas chromatography. Five-point transects perpendicular to drainage canals provided variation in the depth of water tables for the samples. Data from oil palm fields were compared to data from an adjacent swamp forest. The data confirmed that  the increasing depth of water table was accompanied by the increasing in microbial activity that was measured by CO2 emission.  The CO2 emissions from chambers with additional root zones were higher than from bulk soil chambers between one to four times.
The Changes of P-fractions and Solubility of Phosphate Rock in Ultisol Treated by Organic Matter and Phosphate Rock Djuniwati, Sri; Nugroho, Budi; Pulunggono, Heru Bagus
JOURNAL OF TROPICAL SOILS Vol. 17 No. 3: September 2012
Publisher : UNIVERSITY OF LAMPUNG

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.5400/jts.2012.v17i3.203-210

Abstract

Phosphorus (P) is one of the essential elements for plant, however, its availability is mostly very low in acid soils. It is well documented that application of phosphate rock and organic matter are able to change the level of availability of P-form in acid soils.  The objective of the research were to evaluate the changes of P-fractions ( resin-P, NaHCO3-Pi, and NaHCO3-Po) and phosphate rock dissolution which were induced by application of organic matter (Imperata cylindrica, Pueraria javanica, dan Colopogonium mucunoides) and phosphate rock in Utisol Lampung.  The experiment was designed in a completely randomized design with three factors and three replications.  The first factor was the types of organic matter (I. cylindrica, P. javanica, and C. mucunoides), the second factor was the rate of organic matter (0, 2.5, and 5%), and the third factor was the rate of phosphate rock (0, 40, and 80 mg P kg-1).  The results showed that in the  rate of 0 and 1% organic matter, the type of organic matter did not affect P-fraction of NaHCO3-Pi, but in the rate of 2.5 and 5%,  NaHCO3-Pi due to application of  P. javanica, and C. mucunoides higher than due to application of  I. cylindrica.  However, the increasing rate of organic matter increased NaHCO3-Pi. Then, P-fraction of Resin-Pi was affected by the type of organic matter, the rate of  organic matter, and the rate of phosphate rock, respectively. P-fraction of resin-Pi due to application of P.  javanica, and C. mucunoides was higher than due to application of  I. cylindrica, but the effect of  P. javanica, and C. mucunoides was not different.  Increasing the rate of organic matter and phosphate rock increased P-fraction of resin-Pi and NaHCO3-Pi, but P-fraction of NaHCO3-Po was not affected by all treatments.  Meanwhile, dissolution of phosphate rock was affected by the kind of organic matter and soil reaction.  In the rate of 5% organic matter, dissolution of  phosphate rock by application of                                     I. cylindrica (70%) was higher than P. javanica (26.6%), and C.  mucunoides (33.5%), but in the rate of 1%, the effect of I. cylindrica , P. javanica, and C. mucunoides were not different.Keywords: C. mucunoides; I. cylindrica; P. javanica; phosphate rock; P-fractions[How to Cite: Djuniwati S, B Nugroho, and HB Pulunggono. 2012. The Changes of P-fractions and Solubility of Phosphate Rock in Ultisol Treated by Organic Matter and Phosphate Rock. J Trop Soils, 17: 203-210. doi: 10.5400/jts.2012.17.3.203][Permalink/DOI: www.dx.doi.org/10.5400/jts.2012.17.3.203]