1,721,595 research outputs found
Kajian Sifat Fisika Tanah Gambut pada Lahan Rawa dan Beberapa Jenis Lahan dengan Tanaman Berbeda di Kabupaten Bengkalis Provinsi Riau
No full textPOPI POSMARIA : Kajian Sifat Fisika Tanah Gambut Pada Lahan Rawa dan Beberapa Jenis Lahan dengan Tanaman Berbeda di Kabupaten Bengkalis Provinsi Riau. Dibimbing oleh DELIMA LAILAN SARI NASUTION
Kajian tentang tanah gambut ini di lakukan dalam rangka usaha pengembangan lahan gambut sebagai lahan pertanian. Penelitian ini bertujuan untuk mengindentifikasi sifat fisika tanah gambut pada lahan rawa dan beberapa jenis lahan dengan tanaman berbeda untuk mengetahui potensi dari lahan gambut untuk budidaya. Penelitian ini menggunakan metode deskriptif eksploratif secara langsung pada lokasi penelitian dan dilanjutkan dengan pengambilan sampel untuk bahan analisis di laboratorium dengan parameter-parameter penelitian yang meliputi kematangan gambut, warna tanah, kedalaman muka air tanah, kerapatan massa tanah, kerapatan partikel tanah, kadar air dan bahan organik tanah. Penelitian dilakukan di Kabupaten Bengkalis Provinsi Riau dengan luas masing-masing lahan 6 meter, 4 meter dan 3 meter. Analisa sifat fisika tanah dilakukan di laboratorium tanah Fakultas Pertanian Universitas Riau.POPI POSMARIA : Study of Physical Properties on Peat Soil and Several Types Cultivation on Marshland in Bengkalis Regency, Riau Province. Supervised by DELIMA LAILAN SARI NASUTION
Study on Peat Soil was Carried Out in the context of developing Peat Lands as Agricultural Land. This research was aimed to identify the physical properties on peat soil and Several Types Cultivation to find out the potential of peatland for cultivation. This research used exploratory descriptive method directly at the test site and proceed it with sampling for material analysis in laboratories which includes the level of maturity of peat, soil color, depth groundwater, bulk density, partikel density, groundwater level, organic matter. The research was carried out in Bengkalis Regency Riau Province the with an area of 6 meters, 4 meters and 3 meters. The soil physical analysis done in the laboratory of soil physics the Faculty of Agriculture Riau University.62 HalamanSkripsi Sarjan
ANALISIS SISTEM INFORMASI AKUNTANSI PEMBERIAN PEMBIAYAAN PADA PT. FIF (FEDERAL INTERNATIONAL FINANCE) PEKANBARU
No full textABSTRAK
ANALISIS SISTEM INFORMASI AKUNTANSI PEMBERIAN PEMBIAYAAN PADA PT. FIF (FEDERAL INTERNATIONAL FINANCE) PEKANBARU
OLEH:
NURHAPNI LAILAN
01770423510
Tujuan penelitian ini adalah menganalisis sistem informasi akuntansi pemberian pembiayaan pada PT. Federal International Finance Pekanbaru. Penelitian ini dilakukan pada PT. Federal International Finance Pekanbaru yang beralamat di Jalan Soekarno Hatta (arengka 1) no 31-32. Dalam pemberian pembiayaa PT. Federal Internasional Finance menetapkan beberapa prosedur kepada nasabahnya dimulai dari memeriksa kelengkapan dokumen/persyaratan calon debitur, melakukan checking BI,melakukan wawancara langsung dengan calon debitur, survey ke dealer, memesan barang yang di inginkan calon debitur dan dilaksanakan penandatanganan perjanjian kontrak. Hasil penelitian menunjukan bahwa prosedur pemberian pembiayaan pada sistem informasi akuntansi pada PT. Federal International Finance Pekanbaru telah sesuai dengan standar sistem informasi akuntansi pemberian pembiayaan pada umum nya karena telah memenuhi unsur-unsur fungsi yang terkait dalam sistem informasi akuntansi, mengempulkan data, mengolah data menjadi informasi serta mendistribusikan informasi tersebut kepada pengguna.
Kata kunci: Sistem Informasi, Akuntansi, Pembiayaa
Aplikasi Model Hidrologi F J Mock untuk Menghitung Debit Bulanan Sub DAS Sei Petani
No full textFriska Veronika Ulina Simanjuntak : Aplikasi Model Hidrologi F J Mock Untuk Menghitung Debit Bulanan Sub DAS Sei Petani, dibimbing oleh Delima Lailan Sari Nasution.
Perencanaan hidrologi selalu berkaitan dengan karakteristik daerah aliran sungai (DAS). Dimana karakteristik DAS tersebut sangat berpengaruh terhadap kondisi debit aliran sungai. Dalam upaya untuk pengembangan sumber daya air diperlukan data debit sungai dengan jangkauan data yang panjang dan lengkap. Dalam kaitan ini diperlukan suatu sistem model hidrologi untuk mengalihragamkan suatu masukan karakteristik daerah pengaliran sungai tertentu menjadi keluaran debit. Tujuan dari penelitian ini adalah untuk mendapatkan nilai debit Sub DAS Sei Petani menggunakan model Mock. Uji ketelitian model Mock dilakukan dengan cara proses kalibrasi dan verifikasi yang menunjukkan bahwa model tersebut layak diaplikasikan pada Sub DAS Sei Petani yang ditandai dengan hasil keluaran nilai koefisien korelasi (r) dan volumen error (VE). Hasil penelitian model Mock memprediksikan bahwa indikator kesehatan DAS (Q maks, Q min, dan koefisien regim sungai) Sub DAS Sei Petani dalam kondisi yang baik. Rataan debit simulasi tertinngi ialah 3,416 m3/s , sedangkan debit terendah ialah 0,770 m3/s dengan nilai KRS sebesar 4,468.Friska Veronika Ulina Simanjuntak: Hydrological Application of F J Mock Model to Calculate Monthly Sei Petani Sub Watershed Discharge, guided by Delima Lailan Sari Nasution.
Hydrological planning is always related to watershed characteristicof river discharge data with a hydrological model system to deversity an input of a particular watershed characteristic into a discharge output. The purpose of this study is to estimate the discharge value of Sei Petani Sub Watershed using Mock hydrology. The Mock model accuary test was carried out by means of a colaboration and verification process which showed that the model was feasible to be applied to the Sei Petani Sub – watershed which was marked by the output walues of coefficient correlation (r) and volumen error (VE). Hasil penelitian model Mock memprediksikan bahwa indikator kesehatan DAS (Q max, Q min, river regim condition) Sub DAS Sei Petani dalam kondisi yang baik. Rataan debit simulasi tertinngi ialah 3,416 m3/s , sedangkan debit terendah ialah 0,770 m3/s dengan nilai KRS sebesar 4,468.64 HalamanSkripsi Sarjan
Aplikasi Model Hidrologi F J Mock untuk Menghitung Debit Bulanan Sub DAS Sei Petani
No full textFriska Veronika Ulina Simanjuntak : Aplikasi Model Hidrologi F J Mock Untuk Menghitung Debit Bulanan Sub DAS Sei Petani, dibimbing oleh Delima Lailan Sari Nasution.
Perencanaan hidrologi selalu berkaitan dengan karakteristik daerah aliran sungai (DAS). Dimana karakteristik DAS tersebut sangat berpengaruh terhadap kondisi debit aliran sungai. Dalam upaya untuk pengembangan sumber daya air diperlukan data debit sungai dengan jangkauan data yang panjang dan lengkap. Dalam kaitan ini diperlukan suatu sistem model hidrologi untuk mengalihragamkan suatu masukan karakteristik daerah pengaliran sungai tertentu menjadi keluaran debit. Tujuan dari penelitian ini adalah untuk mendapatkan nilai debit Sub DAS Sei Petani menggunakan model Mock. Uji ketelitian model Mock dilakukan dengan cara proses kalibrasi dan verifikasi yang menunjukkan bahwa model tersebut layak diaplikasikan pada Sub DAS Sei Petani yang ditandai dengan hasil keluaran nilai koefisien korelasi (r) dan volumen error (VE). Hasil penelitian model Mock memprediksikan bahwa indikator kesehatan DAS (Q maks, Q min, dan koefisien regim sungai) Sub DAS Sei Petani dalam kondisi yang baik. Rataan debit simulasi tertinngi ialah 3,416 m3/s , sedangkan debit terendah ialah 0,770 m3/s dengan nilai KRS sebesar 4,468.Friska Veronika Ulina Simanjuntak: Hydrological Application of F J Mock Model to Calculate Monthly Sei Petani Sub Watershed Discharge, guided by Delima Lailan Sari Nasution.
Hydrological planning is always related to watershed characteristicof river discharge data with a hydrological model system to deversity an input of a particular watershed characteristic into a discharge output. The purpose of this study is to estimate the discharge value of Sei Petani Sub Watershed using Mock hydrology. The Mock model accuary test was carried out by means of a colaboration and verification process which showed that the model was feasible to be applied to the Sei Petani Sub – watershed which was marked by the output walues of coefficient correlation (r) and volumen error (VE). Hasil penelitian model Mock memprediksikan bahwa indikator kesehatan DAS (Q max, Q min, river regim condition) Sub DAS Sei Petani dalam kondisi yang baik. Rataan debit simulasi tertinngi ialah 3,416 m3/s , sedangkan debit terendah ialah 0,770 m3/s dengan nilai KRS sebesar 4,468.64 HalamanSkripsi Sarjan
Analisa Laju Erosi dan Sedimentasi pada Kawasan Sub DAS Sei Petani
No full textNOVITASARI SIHITE. Analysis of erosion and sedimentation rates in the Sei
Petani Sub-watershed area, guided by DELIMA LAILAN SARI NASUTION.
Erosion and sedimentation are the processes of releasing soil grains from their
parent in a place and the lifting of the material by water or wind movements
followed by deposition. This study aims to calculate the amount of soil erosion
and sedimentation in the sub-watershed area of sei farmers. The method used in
this study is to collect primary data and secondary data, namely rainfall data for
the last 10 years of fortune stations, water level data, data on physical properties
of soil and data on river discharge and sediment discharge using discharge
equations. From the results of the study, the value of erosion that occurred in the
Sei Petani Sub-watershed area for observation points I, II, III, IV, V, VI, VII, VIII
were 11.49 ton / (ha.thn), 1,19 ton / (ha.thn), 1037,70 ton / (ha.thn), and 20.34
tonnes / (ha.thn), 11,92 tonnes / (ha.thn), 1.24 tonnes / (ha. yr), 1077,38 tonnes /
(ha.thn) and 21.12 tonnes / (ha.yrs) while the results of the sedimentation rate in
the rainy season are 300,2183 tonnes / day, dry season 39,77 tonnes / day and for
sedimentation basis of 256854,24 tonnes / day.NOVITASARI SIHITE. Analisis laju erosi dan sedimentasi pada kawasan Sub
DAS Sei Petani, dibimbing oleh DELIMA LAILAN SARI NASUTION.
Erosi dan sedimentasi merupakan proses terlepasnya butiran tanah dari
induknya di suatu tempat dan terangkatnya material tersebut oleh gerakan air atau
angin kemudian diikuti dengan pengendapan. Penelitian ini bertujuan untuk
menghitung besarnya erosi tanah dan sedimentasi pada kawasan Sub DAS sei
petani. Metode yang dilakukan pada penelitian ini adalah dengan mengumpulkan
data primer dan data sekunder yaitu data curah hujan 10 Tahun terakhir stasiun
tuntungan, data tinggi muka air, data sifat fisik tanah serta data debit sungai dan
debit sedimen dengan menunggunakan persamaan debit. Dari hasil penelitian
menunjukkan besarnya nilai erosi yang terjadi pada kawasan Sub DAS Sei Petani
untuk titik pengamatan I, II, III, IV, V, VI, VII, VIII berturut-turut yaitu 11,49
ton/(ha.thn), 1,19 ton/(ha.thn), 1037,70 ton/(ha.thn) dan 20,34 ton/(ha.thn), 11,92
ton/(ha.thn), 1,24 ton/(ha.thn), 1077,38 ton/(ha.thn) dan 21,12 ton/(ha.thn)
sedangkan untuk hasil nilai debit sedimen pada musim kemarau sebesar 39,77
ton/hari dan pada musim hujan diperoleh 300,2183 ton/hari dan untuk sedimentasi
dasar sebesar 256854,24 ton/hari.82 HalamanSkripsi Sarjan
Kajian Tingkat Bahaya Erosi (TBE) Tanah Andepts pada Pengunaan Lahan Tanaman Kacang Tanah di Kebun percobaan Kwala Bekala USU
No full textDELIMA LAILAN SARI NASUTION: The Study of Erosion Hazard Level (TBE) of Andepts Soil on Peanut Cultivation at Kwala Bekala Research Field University of North Sumatra, supervised by SUMONO and EDI SUSANTO. Land with a high slope will increase landslide potential if converted into agriculture field without conservation. Therefore, research was carried out at peanut crop area with 15,5 percent landslope during Mei to August 2010 using the USLE and small square methods. The observed parameters were the kind of soil, the effective depth of soil, soil permeability, soil C-organic content, soil texture, soil structure, slope and rainfall. The results showed that the grades of erosion using USLE methods was 103,99 ton/(ha.year) and the average of erosion that occurred according small square methods was 56,52 ton/(ha.year) that was smaller than the USLE method.69 HalamanSkripsi Sarjan
Going Beyond Counting First Authors in Author Co-citation Analysis
No full textThe present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation
counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings
are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that
only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into
account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed
Penentuan Nilai Koefisien Tanaman dari Beberapa Spesies Tanaman Hortikultura pada Tanah Inceptisol dengan Pembenahan Kompos
No full textNURUL TRI RAHMADHANI: Determination of the value of plant coefficients of
several species of horticultural plant on inceptisol soil by composting, supervised
by SUMONO and DELIMA LAILAN SARI NASUTION.
The magnitude of evapotranspiration value of plant can be determined
based on the potential evaporation value and the plant coefficient for each species
from its growth period. This research was aimed to determine the plant coefficient
values of Pakcoy (Brassica rapa L.), Caisim (Brassica juncea L.), and Lettuce
(Lactuca sativa L.) on Inceptisol soil with the addition of compost.
The results showed that the soil texture of each planting medium was
sandy loam, with the ranges of organic materials content of 6,25-5,89%, the
ranges of porosity were 53,87-52,95%, moisture capacity for each plants (Pakcoy,
Caisim, and Lettuce) were 46,46%, 44,31%, and 47,87%, dry weight of each
plants (Pakcoy, Caisim, and Lettuce) were 75 gr, 85 gr, and 35 gr, and then the
value of the plant coefficient for Pakcoy, Caisim and Lettuce in the middle period
of growth (16-30 days) were 0,44; 0,60 and 0,50. As well as the value of the plant
coefficient of Pakcoy, Caisim and Lettuce in the final phase of growth
(31-45 days) were 0,30; 0,31 and 0,44.147 HalamanSkripsi Sarjan
Penentuan Nilai Koefisien Tanaman dari Beberapa Spesies Tanaman Hortikultura pada Tanah Inceptisol dengan Pembenahan Kompos
No full textNURUL TRI RAHMADHANI: Determination of the value of plant coefficients of
several species of horticultural plant on inceptisol soil by composting, supervised
by SUMONO and DELIMA LAILAN SARI NASUTION.
The magnitude of evapotranspiration value of plant can be determined
based on the potential evaporation value and the plant coefficient for each species
from its growth period. This research was aimed to determine the plant coefficient
values of Pakcoy (Brassica rapa L.), Caisim (Brassica juncea L.), and Lettuce
(Lactuca sativa L.) on Inceptisol soil with the addition of compost.
The results showed that the soil texture of each planting medium was
sandy loam, with the ranges of organic materials content of 6,25-5,89%, the
ranges of porosity were 53,87-52,95%, moisture capacity for each plants (Pakcoy,
Caisim, and Lettuce) were 46,46%, 44,31%, and 47,87%, dry weight of each
plants (Pakcoy, Caisim, and Lettuce) were 75 gr, 85 gr, and 35 gr, and then the
value of the plant coefficient for Pakcoy, Caisim and Lettuce in the middle period
of growth (16-30 days) were 0,44; 0,60 and 0,50. As well as the value of the plant
coefficient of Pakcoy, Caisim and Lettuce in the final phase of growth
(31-45 days) were 0,30; 0,31 and 0,44.147 HalamanSkripsi Sarjan
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