Judul: Prediksi Aliran Permukaan pada DAS Mikro Bungku dan DAS Batang Tabir, Provinsi Jambi Menggunakan Model SCS-CN.
Abstrak: The interaction between human and biophysical condition, which include making changes and regulating landuse in order to fulfil their needs can nevertheless destruct the hydrological function of watershed. A Good hydrological function achieved if there is an equilibrium water system to prevent the water shortages in the dry season or water excess in the rainy season. The analysis of the water system is required to determine the impact of the landuse changes. Therefore, it is necessary to conduct a simulation process that makes the water system in a watershed can be learned in a more simple way. The simulation and simplification process is developed in various models. The use of the model certainly has its own limitations and advantages due to the data availability. One of the models used to predict the overland flow in a watershed is a Soil Conservation Service model - Curve Number (SCS-CN). This is a rainfall-runoff model developed by United States Department of Agriculture (USDA), using rainfall data, soil texture, vegetation, initial abstraction as the input and overland flow as the output. Thus, this research aims at: (1) Assessing the biophysical and hydrological characteristics of land in Bungku micro watershed and Batang Tabir watershed, and 2) Predicting the overland Low data by using the Soil Conservation Service - Curve Number (SCS-CN). The study was conducted in two different watershed areas, namely in Bungku micro watershed with 14.02 hectare square, located in Bungku the Village, Bajubang sub District, Batanghari district, and in Batang Tabir watershed with an area of 107 442.86 hectares square located in Merangin, Bungo and Kerinci district. Data collection was conducted from January 2013 as the primary gathered in Bungku micro watershed November 2013 - January 2014, while in Batang Tabir watershed was held in February - March 2014. The result of this research showed that Bungku micro watershed has a hilly and valley terrain conditions characterized by the dominant slope which is a steep slope with a landcover an area consisting of 1.16 hectare square forest and oil palm plantations with a different undercover vegetation, such as coarse grass (2.09 hectare square), shrubs (7.12 hectare square), and bare land (3.65 hectare square). The Distribution of soil texture in this location is quite varied with clay loam (46%) as dominant texture, followed by loam (24%), and clay (21%). Based on the type of soil texture and infiltration that occurs in this area, the dominant hydrologic soil group (HSG) in Bungku micro watershed is group D with the average value of Antecedant Moisture Condition (AMC) which is in the condition I during field observation and having CN varies between grades 73-88. The highest daily rainfall is 64.34 mm while the lowest si 1.95 mm. The result of the highest prediction overland flow of the model is on December 6th, 2013 in 43.11 mm by 58.49 mm rainfall while the lowest is on December 5th, 2013, as high as 0.12 mm with 4.55 mm rainfall. Batang Tabir watershed exhibits various type of landuse compared with Bungku micro watershed, ie forest (67.81%), Mixed Garden (5.16%), oil palm plantation
Keyword: landuse, SCS-CN model, overland flow

Judul: Discharge and Sedimentation Prediction by MWSWAT Model In Upper Citarum Sub-Watershed, West Java Province
Abstrak: This research was conducted in Upper Citarum Watershed – Majalaya region, West Java province within 20 520.71 ha area, from Desember 2010 - June 2011. The main objectives of this study were: (1) to calibrate MWSWAT model using local data, (2), to predict discharge and sediment as hydrological response of land use condition using MWSWAT calibrated model and (3) to simulate MWSWAT calibrated model on several land use conditions. Spatial analysis showed 9 land use classifications were identified on Majalaya, such as: forest, industrial, residential, orchard, estate crops, agricultural land, pasture, paddy field, and shrubland. Farmland on Majalaya was dominated by vegetables (corn, leek, cassava, carrot, cabbage, potatoes and garlic), flowers and paddy. Simulation with MWSWAT calibrated model with climate data of May to December 2001 showed an accurrate and satisfy result with Nash-Sutcliffe Efficiency (NSE) 0.54 and R2 0.69 for discharge prediction and R2 0.77 and NSE 0.51 for sediment prediction. Calibration proccess was done by adjusting 12 parameters which consists of 8 discharge parameters (OV_N, CN2, SOL_AWC, SOL_K, GW_DELAY, ESCO, ALPHA_BF and CH_K2), and 4 sediment parameters (LAT_SED, SPEXP, SLSSUBBSN, and USLE_P). The calibrated MWSWAT model was used to simulate land use 1994 and 2005 with climate conditions based on 2001. The simulation result showed that the land use 1994 had the lowest water yield (43.41 mm) and sediment yield 0.026 t/ha. Land use 2001 had the highest water yield (44.11 mm) and the lowest sediment yield (0.020 t/ha). Meanwhile, land use 2005 showed water yield 44.05 mm and sediment yield 0.10 t/ha. By comparing land use series 1994, 2001 and 2005, the results showed that several land use changes were happening. A lot of forest area were converted to plantation, orchard and agricultural land and it changed surface roughness, curve number (CN), and also crop factor (C), support practice factor (P), and soil erodibility factor (K) of USLE.
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Judul: Trichomonas Gallinae Penyebab Trichomonosis Pada Unggas
Abstrak: Trichomonas gallinae adalah protozoa yang bergerak aktof dengan keempat flagella yang mempunyai layar dan pada salah satu sisinya terdapat membran seperti sirip ikan yang berombak. Spesies dari genus Trichomonas ini mempunyai arti penting pada unggas, karena dapat menyebabkan infeksi pada alat pencernaan bagian atas.
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