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All Journal Jurnal Agrista Jurnal Floratek Proceedings of Annual International Conference Syiah Kuala University - Life Sciences & Engineering Chapter Jurnal Manajemen Sumberdaya Lahan Jurnal Penelitian Pendidikan IPA (JPPIPA) Jurnal Irigasi Jurnal Agroristek Prosiding Seminar Nasional Biologi, Teknologi dan Kependidikan (Biotik) Aceh International Journal of Science and Technology Jurnal Ilmiah Mahasiswa Pertanian Rona Teknik Pertanian

Hairul Basri

Universitas Syiah Kuala

Author-ID : 241202

Agriculture, Biological Sciences & Forestry Biochemistry, Genetics & Molecular Biology Chemical Engineering, Chemistry & Bioengineering Chemistry Civil Engineering, Building, Construction & Architecture Control & Systems Engineering Decision Sciences, Operations Research & Management Dentistry Earth & Planetary Sciences Education Energy Engineering Environmental Science Immunology & microbiology Languange, Linguistic, Communication & Media Library & Information Science Materials Science & Nanotechnology Medicine & Pharmacology Neuroscience Nursing Physics Public Health Social Sciences Other

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Perubahan Beberapa Sifat Fisika dan Kimia Gambut Jambo Aye - Aceh Utara Akibat Perlakuan Berbagai Kedalaman Drainase Hairul Basri; M. Rusli Alibasyah; Lilis Indriansyah
Jurnal Agrista Vol 10, No 1 (2006): Volume 10 Nomor 1 April 2006
Publisher : Fakultas Pertanian, Universitas Syiah Kuala

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Change of Some Phisycial and Chemical Properties of Peat Soil of Jambo Aye- Aceh Utara and due to Depths of Dranage TreatmentABSTRACT. The objective of this research was to evaluate the change of physical and chemical properties of peat soil of Jambo Aye Aceh Utara due to the depth of drainage treatments. The research was set according to randomized completely design with three replication. Pipes of alluminium with length of 100 cm and diameter of 30 cm was used to set the depth of drainage treatments. The depth of drainage treatments were: no-drainage, 20 cm, 40 cm, and 60 cm. The results showed the dept of drainage on peat soil affected some of physical and chemical properties of peat soil. From the physical properties point of view, the deeper of drainage was conducted, the more subsidence occurred, otherwise the higher bulk density was occurred. From the chemical properties point of view, the drainage more than 20 cm decreased pH, N-total, P-available, K-exchangeable, and Base Saturated, otherwise increased C-organic, Cation Exchangeable Capacity, and Al-exchangeable. It was recommended to use the drainage depth of 20 cm for controlling the change of some physical and chemical properties of peat soil.

Pengembangan Metode Prediksi Produksi Air DAS untuk Sungai-sungai Utama di Aceh Husnan Husnan; Hidayat Pawitan; Gatot Irianto; Kukuh Murti Laksono; Hairul Basri
Jurnal Agrista Vol 12, No 3 (2008): Volume 12 Nomor 3 Desember 2008
Publisher : Fakultas Pertanian, Universitas Syiah Kuala

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Developing Prediction Method of Watershed for Main Rivers in AcehABSTRACT. The conversion of rural land to urban land usually increases erosion, discharge and volume of storm runoff in watershed. It also causes other problem that effect soil and water. An urban or urbanizing watershed is one in which impervious surface cover or will soon cover a considerable area. Impervious surface includes roads, side walk, parking lots and building. Natural flow paths in the watershed may be replaced or supplemented by paved gutters, storm sewers or other elements of artificial drainage. Hydrologic studies to determine runoff and peak discharge should ideally be base on long-term stationary stream flow records for the area, such records are seldom available for small drainage areas. Even were they are available, accurate statistical analysis of them is usually impossible because of the conversion of land to urban uses during period of record. It therefore is necessary to estimate peak discharge with hydrologic models based on measurable watershed characteristics. Only through understanding of these characteristic and experience in using these models can be make sound judgments on how to alter model parameter to reflect changing watershed conditions.

SIFAT TANAH DAN AIR YANG TERPENGARUH TSUNAMI DI KECAMATAN LHOKNGA KABUPATEN ACEH BESAR Syakur Syakur; Hairul Basri; Sufardi Sufardi; Muhammad Hatta
Jurnal Floratek Vol 7, No 1 (2012)
Publisher : Program Studi Agroteknologi, Fakultas Pertanian, Universitas Syiah Kuala

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Lhoknga Sub District was one of regions experiencing earthquake and tsunami disaster occurred on 26 December 2004. The aims of the research were to evaluate soil characteristics, to study land suitability and to propose recommendation of land use and rehabilitation of the tsunami affected agricultural area in Lhoknga Sub District. The result showed that soil textures were varied from very coarse at the area near to the coastline to rather fine at the area far from the coast. The soil structures of topsoil was generally plate and blocky, while that of subsoil was generally massive. The quality of irrigation water in was still suitable for crops, the pH of water was neutral and low in salinity (0,4 mS cm-1). The water quality of wells was high (good) and water quality of drainage and surface water was low (rather bad). Water quality of wells was good enough, indicated by low water salinity (0,26-0,78 mS cm-1) and low of SAR value. The recommendations for land reclamation were (1) cleaning and repairing of irrigation and drainage channel (2) leaching of salinity in topsoil from soil profile by flooding method (basin irrigation) or furrow irrigation, (3) constructing the ditches for cultivation in managing the excess of salinity, (4) establishing ditches for paddy, and (5) removing the sediment above the topsoil.

INTERSEPSI AIR HUJAN PADA TANAMAN KOPI RAKYAT DI DESA KEBET, KECAMATAN BEBESEN, KABUPATEN ACEH TENGAH Hairul Basri Basri; Manfarizah Manfarizah; Andi Salasa
Jurnal Floratek Vol 7, No 1 (2012)
Publisher : Program Studi Agroteknologi, Fakultas Pertanian, Universitas Syiah Kuala

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The purpose of the study was to determine the amount of rainfall interception on coffee plants, and obtain a relationship between rainfall and interception of coffee plant. The research was conducted in a coffee plantation in Kebet Village, Bebesen Sub-District, Central Aceh District. The experiment was carried out from February to March 2011. The method used in this research was a descriptive method, using direct measurements in the field. The samples of coffee plants were 4 years and 15 years old. The results showed that rainfall interception of 4 years-coffee-crop was 56.87% of the total rainfall of 82.50 mm and that of 15-year-old coffee plants was 72.12%, of total rainfall of 133.50 mm. The greater the rainfall was, the greater the interception would be, as well as the older age of the coffee plant was, the greater the percentage of interception was recorded. The average proportion of rainfall as the water passes (throughfall) was greater than the proportion of rainfall that becomes stream stems (stemflow), due to high density of leaves covering the stem. Relationship between rainfall and interception on coffee plants was a natural logarithm equation: (1) for 4 years coffee crop, I = 3.440 ln (Pg) + 0.650 and R2 = 0.56; (2) for 15 years old coffee crop, I = 2.992 ln (Pg) + 2.371 and R2 = 0.69.

SIFAT-SIFAT TANAH DAN AIR YANG TERPENGARUH TSUNAMI DI KECAMATAN LHOONG KABUPATEN ACEH BESAR Hairul Basri; Syakur Syakur; Alfian Rusdi
Jurnal Floratek Vol 6, No 2 (2011)
Publisher : Program Studi Agroteknologi, Fakultas Pertanian, Universitas Syiah Kuala

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ABSTRACT The aims of the research were to evaluate soil characteristics, to study land suitability and to propose recommendation of land use and rehabilitation of the tsunami affected agricultural area in Lhoong Sub-District. The result showed that soil textures were varied from very coarse at the area near the coastline to rather fine at the area far from the coast. The soil structures of topsoil were generally plate and blocky, and at subsoil generally massive. The quality of irrigation water in Sub District of Lhoong was still suitable for crops. The pH of water was neutral and low in salinity (0, 4 mS cm-1). The recommendations for land of class A were (1) cleaning and repairing of irrigation and drainage channel, (2) leaching of salinity in topsoil from soil profile by flooding method (irrigation basin) or furrow irrigation, (3) making the ditches for cultivation in managing the excess of salinity, (4) establishing ditches for paddy, and (5) requiring a specified amount of water for the leaching processes and the amount of water required for crops. The recommendation for land class B were (1) cleaning and repairing of irrigation and drainage channel, (2) removing the sediment above the topsoil, (3) leaching the salt from topsoil passing soil profile by irrigation water, (4) constructing ditches for cultivation in managing the excess of salinity.

How to restore the Tropical Peat Swamp Forest in Aceh Province, Indonesia Hairul Basri; . Sufardi; . Sugianto; Syamaun A. Ali; . Khairullah; Ahmad Reza Kasuri
Proceedings of The Annual International Conference, Syiah Kuala University - Life Sciences & Engineering Chapter Vol 5, No 2 (2015): Life Sciences
Publisher : Syiah Kuala University

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This study aims to describe the condition of Tripa Peat Swamp Forest (TPSF) in the Province of Aceh Indonesia that has been converted from forest to oil palm plantation and mixed farms. The results showed that the degradation of the peat soil and the environment have occurred in the TPSF. Degradation of peat is characterized by the occurrence of changes in water holding capacity and changes in chemical and physical properties of soil. Environmental degradation is characterized by changes in groundwater levels and land subsidence. TPSF restoration efforts can be carried out in accordance with the directives of land use and land conservation and water management

Hidrodinamika dan Produk Sedimen terhadap Bendung Irigasi Keumala, Sungai Krueng Baro, Provinsi Aceh Azmeri Azmeri; Hairul Basri; Devi Sundary; Yusni Eva Cus Endang; Faris Zahran Jemi
Jurnal Irigasi Vol 15, No 1 (2020): Jurnal Irigasi
Publisher : Balai Teknik Irigasi

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31028/ji.v15.i1.1-14

Keumala Dam is built on Krueng Baro River which is one of the strategic rivers in Aceh Province to irrigates the farmland and supplies drinking water for the community downstream. However, this river has a considerable issues due to its long path and passing through various geological formations, causing a high concentration of sediments in the river. Therefore, this study aimed to analyze the river hydrodynamics employing the HEC-RAS 5.0 software. The results of the study revealed that the flow capacity of sediment transport along the riverbed varies directly with the difference between the shear stress at the bottom sediment and the critical shear stress allowed for moving particles. Sediment transport occurred in all sediment samples from the upstream and downstream of Keumala Dam. The flow reduction due to the damming changed the channel and flow regime, while the decrease in water release reduced the floating and bottom sediment transport to the the downstream. The total sediment around the weir area at the normal discharge is 6,325,698.93 tons/year. Sedimentation around the weir is a severe problem as it can affect the function and performance of the weir and irrigation channel. Siltation due to sedimentation also closed the intake of Keumala PDAM. Thus, periodical dredging and transporting sediments from the bottom of the weir are necessary to overcome this problem. Dredging and transporting sediments will improve the Keumala weir performance to irrigates the Krueng Baro Irrigation Area. Thus, the discharge capacity of othe weir intake can be maintained to irrigate the farmland following the planned area.

ANALISIS KUALITAS TANAH DAN UPAYA MITIGASI BENCANA HIDROLOGIS DI SUB DAS KRUENG JREUE ACEH BESAR Helmi Helmi; Hairul Basri; Sufardi Sufardi; Helmi Helmi
Prosiding Seminar Nasional Biotik Vol 4, No 1 (2016): PROSIDING SEMINAR NASIONAL BIOTIK IV 2016
Publisher : Prosiding Seminar Nasional Biotik

Alih fungsi lahan menyebabkan penurunan tingkat kesuburan tanah atau semakin rendahnya nilai indeks kualitas tanah (IKT). Penelitian ini bertujuan untuk mengetahui tingkat kualitas tanah pada beberapa jenis penggunaan lahan dengan pendekatan nilai IKT. IKT dihitung berdasarkan kriteria Mausbach & Seybold (1998), yang disesuaikan dengan kondisi lapangan menggunakan analisis Minimum Data Set (MDS). Parameter yang diamati meliputi kedalaman perakaran, tekstur tanah, BVT, porositas total, pH tanah, C-organik, N-total, P-tersedia, K-dd dan respirasi tanah. Hasil penelitian menunjukkan, jenis penggunaan lahan yang berkualitas baik, pemukiman, hutan sekunder dan hutan primer, dengan nilai masing-masing 0,66; 0,62 dan 0,61. Sedangkan padang rumput, tanah terbuka, sawah, tegalan, dan semak belukar berkualitas sedang, dengan nilai masing-masing 0,48; 0,49; 0,52; 0,54 dan 0,54. Implikasi dari penelitian ini, upaya mitigasi bencana hidrologis secara struktural dan non struktural sangat diperlukan untuk meningkatkan dan mempertahankan kualitas tanah secara berkelanjutan.

IDENTIFIKASI PERUBAHAN UNSUR-UNSUR IKLIM TERHADAP PRODUKTIFITAS PADI SAWAH DI KABUPATEN PIDIE JAYA Junaidi, Hairul Basri, Sugianto
Jurnal Agroristek Vol 2, No 2 (2019): Agustus 2019
Publisher : Lembaga Penelitian dan Pengabdian kepada Masyarakat (LPPM) Universitas Jabal Ghafur

Penelitian bertujuan untuk menganalisis perubahan unsur-unsur iklim dan pergeseran musim tanam serta hubungannya terhadap produktifitas hasil tanaman padi secara spasial dalam kurun waktu 10 tahun di Kecamatan Bandar Baru, Bandar Dua dan Meureudu. Penelitian ini bersifat diskriptif yang dititik beratkan pada pengetahuan petani mengenai penerapan musim tanam dan adaptasi petani terhadap perubahan unsur-unsur iklim seperti curah hujan, kelembaban dan suhu wilayah yang dikaji adalah berdasarkan pengalaman petani terhadap permasalahan iklim yang dihadapi saat ini. Jenis data yang diambil adalah data sekunder dari BPP di Kecamatan Bandar Baru, Bandar Dua dan Meureudu dan dari Dinas Pertanian Kabupaten Pidie Jaya. Selanjutnya analisis data menggunakan regresi linier berganda, Y sebagai variabel terikat yaitu produksifitas padi (ton/ha) dan X sebagai variabel bebas yaitu unsur iklim yang berupa curah hujan (X1), kelembaban (X2), suhu (X3) dan musim tanam (X4). Hasil penelitian menunjukkan bahwa rata-rata perubahan iklim di Kecamatan Bandar Baru, Bandar Dua dan Meureudu dalam kurun waktu 10 tahun dapat mempengaruhi hasil rata-rata produktifitas padi sebesar 6,55 ton/tahun dengan total rata-rata curah hujan adalah 1.942,30 mm/tahun, suhu sebesar 27,55 oC dengan penggolongan panas dan kelembaban sebesar 78,23% dengan indek kelembaban basah berdasarkan klasifikasi Douglas H.K. Lee. Rata-rata pergeseran musim tanam gaduh di Kecamatan Bandar Baru selama 22 hari, Bandar Dua selama 20 hari dan meureudu selama 19 hari, akan tetapi terjadi pergeseran rata-rata musim tanam rendengan di Kecamatan Bandar Baru selama 19 hari, Bandar Dua selama 17 hari dan Meureudu selama 18 hari dan berhubungan negatif yang nyata antara pergeseran musim tanam dan perubahan iklim, sehingga tingkat produktifitas padi terjadi penurunan di Kecamatan di Bandar Baru, Bandar Dua dan meureudu dengan nilai koefisien determinasi masing-masing sebesar 46,82 persen, 54,47 persen dan 21,83 persen Kata kunci: unsur-unsur iklim, musim tanam, produktifitas padi.

Development of Rainfall-runoff Modeling Using a Tank Model: Problems and Challenges in Province of Aceh, Indonesia Hairul Basri
Aceh International Journal of Science and Technology Vol 2, No 1 (2013): April 2013
Publisher : Graduate Program of Syiah Kuala University

Abtstract - Rainfall-runoff modeling using tank model founded by Sugawara has been widely used in Asia. Many researchers use the tank model to predict water availability and flooding in a watershed. This paper describes the concept of rainfall-runoff modeling using tank model, discuss the problems and challenges the use of tank model, especially in Province of Aceh, Indonesia and how to improve the outcome of simulation of tank model. Many factors affect the rainfall-runoff phenomena of a wide range of watershed include: soil type, land use types, rainfall, morphometry, geology and geomorphology, caused the tank model usefull only for concerning watershed. It is necessary to adjust some parameters of tank model for other watershed by recalibrating the observed and simulated discharges. Rainfall runoff modeling using the tank model for a watershed scale is more reasonable focused on each sub-watershed by considering soil types, land use types and rainfall of the concerning watershed. Land use data can be enhanced by using landsat imagery or aerial photographs to support the validation the existing of land use type. Long term of observed discharges and rainfall data should be increased by set up the AWLR (Automatic Water Level Recorder) and rainfall stations for each of sub-watersheds. The reasonable tank model can be resulted not only by calibrating the observed and simulated discharges, but also by considering the observed and simulated infiltration for each soil and land use types of the concerning watershed.

Co-Authors . Azmeri, . . Khairullah . Sugianto Abubakar Karim Afriadi Ihsan Ahmad Reza Kasuri Akbar Maulana Al Qarana Alayani, Rifa Alfian Rusdi Ali Muhammad Muslih Amaluddin Amaluddin Andi Salasa Arif Habibal Umam Aris Marta Ashabul Anhar Ashabul Anhar Ashabul Anhar Attabari Aldin Ayu Mulia Ayuseara Putri Gayosia Bintang Bintang Chandra Priadi Dahlan D Dahlan Dahlan Darwin Darwin Deden Nurochman Devi Sundary Dian Permata Alhai Dina Firmadiana Dini Karina Efendi Efendi Eka Aulia Ellyanti Ellyanti Essy Harnelly Fadhi Maireza Putra Fadhli, Rahmad Fajar Rahmah Faris Zahran Jemi Fatimah Aulia Silalahi Fauzi Harun Gatot Irianto Helmi Helmi Helmi Helmi Helmi Helmi Helmi Helmi Hema Hayati Heriadi Dedek Sahputra Herry Andrisa Hidayat Pawitan Husnan Husnan Husni Husni Ichsan Ichsan Ihsan Siddiq Ilham Hanafi Ilham Wijaya Indra Indra Intan Ridha Putri Intan Solehah Ismed Ramadhan Joko Widiyanto Khairini Hasri Khairullah Khairullah Khairun Purgawa Konadi Konadi Kukuh Murti Laksono Layli Nuriani Lilis Indriansyah Lisa Mutia M. Rusli Alibasyah Manfarizah Manfarizah Marisa marisa marisa Maunida Isnin Mhd Rizha Fahlevi Mira Mardhiah Mirza Junianto Mudinillah, Adam Muhammad Aygun Muhammad Hatta Muhammad Rusdi Muhammad Rusdi Muhammad Rusdi Muhammad Rusli Alibasyah Mukhsin Febi Mirza Muzakki Muzakki Niya Putri Utami Nurmala Ramadhani Lubis Oktri Sri Wahyuni Putri Ayuni Arsita Rasyid Alkhoir Lubis Ridha Tiara Suci Rifa Alayani RM Adjie Prakasa Roby Arnando Romano Romano Romi Rinaldi Ryan Moulana Sartika Ningsih Septyan Arief Subhan Subhan Sufardi Sufardi Sufardi Sufardi Sugianto Sugianto Sugianto Sugianto*, Sugianto Sulasutri Sulasutri Syahrul Syahrul Syahrul Syahrul Syahrul Syahrul Syahrul Syahrul Syakur Syakur Syakur*, Syakur Syamaun A. Ali Syamaun A. Ali Syarifah Renny Fauzi T.M. Hadhar Wijaya Teti Arabia Teuku Alvisyahrin Teuku Muhammad Afrizal Yogi Ramadhan Ritonga Yulia Dewi Fazlina Yusni Eva Cus Endang Zainabun Zainabun Zulia Chairani

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