46 research outputs found

    EVALUASI DAN PENENTUAN JENIS TANAH DI KABUPATEN SERAM BAGIAN BARAT EVALUATION AND DETERMINATION OF LAND IN THE DISTRICT OF WEST SERAM

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    Penelitian bertujuan untuk mengidentifikasi tanah di Kabupaten Seram Bagian Barat  Provinsi Maluku, dilaksanakan pada tahun 2013 menggunakan Sistem Klasifikasi  Taksonomi Tanah (Soil Survay Staff, 2010). Dari hasil penelitian ditemukan lima ordo tanah menurunkan sebanyak tujuh sub-ordo, sembilan grup, dan 15 subgrup tanah. Ordo Entisol menurunkan tiga subgroup, yaitu Lythic Udorthents, Typic Udorrthents, dan Typic Quartzipsamments. Ordo Molisols menurunkan dua subgroup, yaitu Lythic Hapludolls dan Typic Hapludolls. Ordo Inceptisol menurunkan tujuh subgroup, yaitu Fluventic Endoaquepts, Vertic Endoaquepts, Typic Endoaquepts, Lythic Dystrudepts, Typic Dystrudepts, Aquic Eutrudepts, dan Typic Eutrudepts. Ordo Alfisols menurunkan satu subgroup, yaitu Typic Hapludalfs. Ordo Ultisols menurunkan dua subgroup, yaitu Typic Paleudults dan Typic Hapludults. Pada umumnya tanah-tanah di daerah penelitian merupakan tanah belum mengalami perkembangan horizon dan memiliki solum tanah dari dangkal sampai dalam. Warna tanah bervariasi dari coklat hinga kuning kemerahan. Tekstur liat sampai berpasir, konsistensi sampai lekat, kedalaman efektif dangkal sampai dalam, dan pH tanah sangat masam sampai agak alkalis. Keadaan landform datar hingga bergunung. The research aims to identify the land in the district of West Seram Maluku Province, carried out in 2013 using Classification System Soil Taxonomy (Soil Survay Staff, 2010). From the results of the study found five orders of soil lowered as much as seven sub-orders, nine groups and 15 subgroups ground. Order of Entisol lowered three subgroups, namely Lythic Udorthents, Typic Udorrthents, and Typic Quartzipsamments. Order of Molisols down two subgroups, namely Lythic Hapludolls and Typic Hapludolls. Order of Inceptisol lowered seven subgroups, namely Fluventic Endoaquepts, Vertic Endoaquepts, Typic Endoaquepts, Lythic Dystrudepts, Typic Dystrudepts, Aquic Eutrudepts, and Typic Eutrudepts. Order of Alfisols lowered one subgroup, ie Typic Hapludalfs. Order of Ultisols down two subgroups, namely Typic Paleudults and Typic Hapludults. In general, the soils in the study area is the land has not been progressing and has solum soil horizon from shallow to deep. Ground color varies from yellow hinga reddish brown. Loamy to sandy texture, consistency until sticky, effective depth of shallow to deep, and very sour soil pH to slightly alkaline. Flat, hilly landform circumstances

    Keragaan Pertumbuhan dan Hasil Tanaman Berbasis Padi Gogo pada Lahan Kering di Maluku

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    Upland rice-based cropping pattern is a form of multiple cropping including intercropping, sequential planting, and relay planting where upland rice as a base crop can be preceded and/or rotated with other food crops as a secondary crop. The research was aimed to provide recommendations for upland rice-based cropping pattern technology in dryland agroecosystems in Maluku that would be able to increase land productivity > 1.00 (MCI = Multiple Cropping Index > 100%) compared to existing cropping patterns. The study used a Randomized Block Design (RCBD) with four treatments and repeated five times (farmers as replications). Four treatments for upland rice-based planting pattern technology assemblies, namely: 1) Pattern-A (Farmer A Pattern); 2) Pattern-B (Farmer B Planting Pattern B); 3) Pattern C (Farmer Improvement Cropping Pattern); and 4) Pattern D (Introduced Plant Pattern). The results showed that upland rice was planted double (multiple cropping) through intercropping and/or sequential cropping, namely Improved Cropping Patterns (Pattern C = Upland Rice + Corn - Peanuts) and Introducing Cropping Patterns (Pattern D = Upland Rice + Corn/Cassava - Green Beans - Peanuts) can increase land productivity with a double-cropping index 1.35 - 1.80 (IPG = 135% - 180%) compared to upland rice grown in monoculture (Farming Patterns). Multiple cropping (Upland Rice + Corn/Cassava - Green Beans - Peanuts) can be recommended as Upland Rice-Based Planting Technology Package on dry land in Maluku, because it can increase land productivity> 1.00 with an MCI (Multiple Cropping Index) of 180%. Keywords: dry land, performance, upland rice   ABSTRAK Pola Tanam berbasis padi gogo merupakan bentuk pola bertanam ganda meliputi tumpangsari, tumpang gilir (runtun) dan tanaman sisipan dimana padi gogo sebagai komoditi pokok (base crop) yang bisa didahului dan atau digilir dengan tanaman pangan lainnya sebagai komoditi ikutan (secondary crop). Tujuan dari penelitian ini adalah untuk mendapatan rekomendasi paket teknologi pola tanam berbasis padi gogo pada agroekosistem lahan kering di Maluku yang mampu meningkatan produktivitas lahan > 1.00 (IPG = Indeks Pertanaman Ganda >100 %) dibandingkan dengan pola tanam petani eksisting. Penelitian menggunakan Rancangan Acak Kelompok (RAK) dengan empat macam perlakuan dan diulang lima kali (petani sebagai ulangan). Empat perlakukan rakitan teknologi pola tanam berbasis padi gogo, yaitu: 1) Pola-A (Pola Tanam Petani A); 2) Pola-B (Pola Tanam Petani B); 3) Pola C (Pola Tanam Petani Perbaikan); dan 4) Pola D (Pola Tanaman Introduksi). Hasil penelitian menunjukkan bahwa padi gogo ditanam secara ganda (multiple cropping) melalui tumpangsari dan atau tumpanggilir, yaitu Pola Tanam Petani Perbaikan (Pola C = Padi Gogo + Jagung - Kacang Tanah) dan Pola Tanam Introduksi (Pola D = Padi Gogo + Jagung/Ubikayu - Kacang Hijau - Kacang Tanah) dapat meningkatkan produktivitas lahan 1.35 – 1.80 (IPG = 135% - 180%) dibandingkan jika padi gogo ditanam secara monokultur (Pola Tanam Petani). Pola bertanam ganda (Padi Gogo+Jagung/Ubikayu - Kacang Hijau - Kacang Tanah) dapat direkomendasikan sebagai Paket Teknologi Pola Tanam Berbasis Padi Gogo pada lahan kering di Maluku, karena dapat meningkatkan produktivitas lahan >1.00 dengan nilai IPG (Indeks Pertanaman Ganda) 180%. Kata Kunci: keragaan, lahan kering, padi gog

    Measurement of the charge ratio of atmospheric muons with the CMS detector

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    This is the pre-print version of this Article. The official published version can be accessed from the link below - Copyright @ 2010 ElsevierWe present a measurement of the ratio of positive to negative muon fluxes from cosmic ray interactions in the atmosphere, using data collected by the CMS detector both at ground level and in the underground experimental cavern at the CERN LHC. Muons were detected in the momentum range from 5 GeV/c to 1 TeV/c. The surface flux ratio is measured to be 1.2766 \pm 0.0032(stat.) \pm 0.0032 (syst.), independent of the muon momentum, below 100 GeV/c. This is the most precise measurement to date. At higher momenta the data are consistent with an increase of the charge ratio, in agreement with cosmic ray shower models and compatible with previous measurements by deep-underground experiments

    Observation of a new Xi(b) baryon

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    The first observation of a new b baryon via its strong decay into Xi(b)^- pi^+ (plus charge conjugates) is reported. The measurement uses a data sample of pp collisions at sqrt(s) = 7 TeV collected by the CMS experiment at the LHC, corresponding to an integrated luminosity of 5.3 inverse femtobarns. The known Xi(b)^- baryon is reconstructed via the decay chain Xi(b)^- to J/psi Xi^- to mu^+ mu^- Lambda^0 pi^-, with Lambda^0 to p pi^-. A peak is observed in the distribution of the difference between the mass of the Xi(b)^- pi^+ system and the sum of the masses of the Xi(b)^- and pi^+, with a significance exceeding five standard deviations. The mass difference of the peak is 14.84 +/- 0.74 (stat.) +/- 0.28 (syst.) MeV. The new state most likely corresponds to the J^P=3/2^+ companion of the Xi(b).Comment: Submitted to Physical Review Letter

    Measurements of inclusive W and Z cross sections in pp collisions at root s=7 TeV

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    This is the pre-print version of the Published Article, which can be accessed from the link below - Copyright @ 2011 Springer VerlagMeasurements of inclusive W and Z boson production cross sections in pp collisions at sqrt(s)=7 TeV are presented, based on 2.9 inverse picobarns of data recorded by the CMS detector at the LHC. The measurements, performed in the electron and muon decay channels, are combined to give sigma(pp to WX) times B(W to muon or electron + neutrino) = 9.95 \pm 0.07(stat.) \pm 0.28(syst.) \pm 1.09(lumi.) nb and sigma(pp to ZX) times B(Z to oppositely charged muon or electron pairs) = 0.931 \pm 0.026(stat.) \pm 0.023(syst.) \pm 0.102(lumi.) nb. Theoretical predictions, calculated at the next-to-next-to-leading order in QCD using recent parton distribution functions, are in agreement with the measured cross sections. Ratios of cross sections, which incur an experimental systematic uncertainty of less than 4%, are also reported

    Measurement of dijet angular distributions and search for quark compositeness in pp collisions at √s=7TeV

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    Dijet angular distributions are measured over a wide range of dijet invariant masses in pp collisions at root s = 7 TeV, at the CERN LHC. The event sample, recorded with the CMS detector, corresponds to an integrated luminosity of 36 pb(-1). The data are found to be in good agreement with the predictions of perturbative QCD, and yield no evidence of quark compositeness. With a modified frequentist approach, a lower limit on the contact interaction scale for left-handed quarks of Lambda(+) = 5.6 TeV (Lambda(-) = 6.7 TeV) for destructive (constructive) interference is obtained at the 95% confidence level

    Transverse-momentum and pseudorapidity distributions of charged hadrons in pp collisions at √s=0.9 and 2.36 TeV

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    Measurements of inclusive charged-hadron transverse-momentum and pseudorapidity distributions are presented for proton-proton collisions at root s = 0.9 and 2.36 TeV. The data were collected with the CMS detector during the LHC commissioning in December 2009. For non-single-diffractive interactions, the average charged-hadron transverse momentum is measured to be 0.46 +/- 0.01 (stat.) +/- 0.01 (syst.) GeV/c at 0.9 TeV and 0.50 +/- 0.01 (stat.) +/- 0.01 (syst.) GeV/c at 2.36 TeV, for pseudorapidities between -2.4 and +2.4. At these energies, the measured pseudorapidity densities in the central region, dN(ch)/d eta vertical bar(vertical bar eta vertical bar and pp collisions. The results at 2.36 TeV represent the highest-energy measurements at a particle collider to date
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