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STUDI LOKASI TITIK-TITIK RENTAN EROSI DI SEPANJANG JALAN SEKITAR BUKIT SELASIH SAMPAI KECAMATAN LUBUK KILANGAN Astuti, Rina Febri Yani; Edial, Helfia; Thesiwati, Aslan Sari
Pendidikan Geografi Vol 2, No 1 (2013): Jurnal Mahasiswa Prodi Pendidikan Geografi
Publisher : STKIP PGRI Sumbar

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The aim of this study: Analyzing the level slope, land cover, rock types, soil types and analyze the existing level of rainfall at various points of erosion along the way Bukit selasih until Kecamatan Lubuk Kilangan. The research methodology is descriptive. Sampling technique based on geological maps Kecamatan Lubuk Kilangan the samples taken by the different rock types and is controlled by the degree of slope and land cover. The results showed that: the rate of slope at any point in the study sample was 35% in sample 1, sample 2 at 30% and 65% in sample 3, thus the third point of the sample had a high attrition rate because it has a steep slope up to very steep. Vegetation or land cover types that exist in the research area is planted with trees a little, shrubs, mosses and open. At each sample point there is always the possibility of erosion. On sample I (Indarung-Lubuk Paraku) with rock types Qf (Quarter fluvial) 5.5 rock hardness and condition weathered rock and soil texture being argillaceous sand, sample II (Lubuk Paraku-Panorama II) with Pcks rock type, rock hardness 8 and lightweight weathered rock conditions, which has the texture of clay soil are dusty and sample III (Panorama II-Lubuk-Selasih) Qtau rock types (Quarter andesites) which condition weathered rock, rock hardness level 2, and have a smooth texture that is loamy soil. In the study area has a high rainfall intensity at any time, the high levels of erosion due to high rainfall levels anyway.
STUDI TINGKAT EROSI DAERAH ALIRAN SUNGAI LUMPO KECAMATAN IV JURAI KABUPATEN PESISIR SELATAN Marnil, Sepka; Edial, Helfia; Juita, Erna
Pendidikan Geografi Vol 2, No 1 (2013): Jurnal Mahasiswa Prodi Pendidikan Geografi
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This research study aims to determine the Watershed Erosion Rate LumpoKecamatan IV Jurai South Coastal District. The method used in this research is descriptive method is to give an idea of the character of the object studied and compared between each other in order to obtain the desired conclusion, sampling method in this study is the method of sample areas (sampling area), where the unit of measurement is each lithological units derived from the geological map with consideration of land use (vegetation cover), slope and soil type. The results showed that: (1) The level of erosion in the study area is divided into 2 parts low Qal.1.Sw.Lat lithological units and lithological units Qal.1.Sm.Lat, while the rate of erosion was the lithological units Tomp.III . Sw.Lat, Tomp.III.Kc.Lat and Tomp.V.Ht.Lat, (2) There were no differences in erosion rate based on land use (agriculture and plantation) in each different lithological units in the watershed Lumpo and (3) there were no differences in erosion rate by land use (agriculture and plantation) in each unit of the same lithology in watershed Lumpo.
OPTIMALISASI PEMANFAATAN LAHAN PEKARANGAN RUMAH DI NAGARI KOTO BARU KECAMATAN LUHAK NAN DUO KABUPATEN PASAMAN BARAT Rahmah, Softi Nur; Edial, Helfia; Yuherman, Yuherman
Pendidikan Geografi Vol 2, No 1 (2013): Jurnal Mahasiswa Prodi Pendidikan Geografi
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This research aimed to obtain information, analyze and discuss data on the optimization the utilization of homestead land in Luhak Nan Duo District Nagari Koto Baru West Pasaman Regency. Type of research was descriptive correlational. The research population was a whole head of the family/ homemakers who has a homestead in Luhak Nan Duo District Nagari Koto Baru West Pasaman Regency. Samples from this research area is a residential region in Nagari Koto Baru by taken three were deemed to represent the ellipse is Jorong Sei. Talang, Jorong Jambak, and Jorong Ophir. Respondent sampling done by used proportional random sampling technigue by taken a sample of 80 respondents and data collection through questionnaire distribution. Based on a simple linear regression analysis, double (multiple) and the correlation it can be concluded as follows: (1) Found the influence of education on the level of optimization the utilization of homestead land in Nan Duo District Nagari Koto Baru West Pasaman Regency because t count > t table ( 6.936 > 2.00), power relations were high (r = 0.618) and the contributions gave 38.1%, (2) Found the spacious homestead land influence toward optimization the utilization of homestead land in Luhak Nan Duo District Nagari Koto Baru West Pasaman Regency because t count > t table (6.809 > 2.00), power relations were high (r = 0.611) and the contributions gave 37.3%, (3) Found the influence of free time toward optimization the utilization of homestead land in Luhak Nan Duo District Nagari Koto Baru West Pasaman Regency because t count > t table (4.685 > 2.00), the strength of the relationship enough category (r = 0.469) and the contributions gave 22% and (4) Found the influence of the level of public education, spacious homestead and free time together toward optimize the utilization of homestead land in Luhak Nan Duo District Nagari Koto Baru West Pasaman Regency because F count > F table (42.778 > 3.96), the strength of the relationship between three variables toward optimize the utilization of homestead in Luhak Nan Duo District Nagari Koto Baru West Pasaman Regency included were high (r = 0.793) and higher contributions gave 62.8%.
PROFIL MASYARAKAT DALAM MEMANFAATKAN AIR BATANG HARI DI KENAGARIAN LUBUK ULANG ALING SELATAN KECAMATAN SANGIR BATANG HARI KABUPATEN SOLOK SELATAN Wati, Ratna; Edial, Helfia; Zuriyani, Elvi
Pendidikan Geografi Vol 2, No 2 (2013): Jurnal Wisuda Ke 47, Pendidikan Geografi
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This study aims to determine the profile of the community in the use of water in Batang Hari river Kenagarian Lubuk Aling Selatan District Sangir Batang Hari Solok Selatan which include : 1) education , 2 ) economic conditions, 3 ) the level of health dan 4 ) culture.This research is descriptive. The population in this study is people in Kenagarian Lubuk Ulang Aling Selatan having ± 20 m distance from their homes to the water Batang Hari totaling 302 households, each household can be represented by one households. Respondent sample taken with the technique of random sampling proportional to the proportion of 25 % so that the sample was 76 families .The research found that : 1 ) the condition of the education level of the people who use water Batang Hari generally never get a formal education with education level taken is not complete primary school - The End SD , although so many are out of school . Considers very important the public education so that the children need to get an education . Currently children who are still studying are generally 1 and there are children who drop out of school , ( 2 ) the economic condition that utilizes water generally is Batang Hari gold miners with income > Rp 5.000.000/bulan . Society also has a side job as a farmer with revenue generally Rp 1,000,000 - Rp 2.000.000/bulan . Society also has a family member that works but needs less fulfilled life , ( 3 ) the condition of public health that utilizes water generally has Batang Hari WC / private bathroom but rarely used . Clean water sources are rivers , water treatment generally boiled water consumed while health is generally decent and ( 4 ) cultural communities like bathing in the river for reasons more to socialize with the people around
Water QualityOf SibakurRodfor Nila Fish Keramba Systems in the Deep Sub TarokVillages LatangSijunjungDistrict Gamiarsih, Elva; Edial, Helfia; Juita, Erna
Pendidikan Geografi Vol 2, No 2 (2013): Jurnal Wisuda Ke 47, Pendidikan Geografi
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Water  Sibakur rod located in deep sub Latang Tarok villages are common water resource that has an important role for the people living around. sibakur stem water use by local people covering different aspects of life. of them as a place of cage fishfarming, fishing area, water the fields, and household activities. purpose of fish farming is to produce fish in larger quantities than the natural life.This study aimed to obtain information, data, analyzes, discusses and discloses: (1) physical condition sibakur system water for nila fish cage systems which include temperature, color, and turbidity (2) water chemistry conditions Sibakurrod for nila fish farming cage systems which included pH, dissolved oxygen (DO), carbondioxide(CO2), phosphates (PO4) and ammonia (NH3).            Type of research is descriptive research. this study to determine the physical and chemical parameters of water were used as SibakurBatang fish farming cage Systems. This study compared the results of the analysis are obtained directly from the field and laboratory with water quality standards for aquaculture. The samples tested were in the region of the upstream, midstream, and downstream water Sibakur Trunk. The results on the physical and chemical parameters tabulated and analyzed descriptively.             Results of the study are as follows: (1) Water Quality Rods Sibakur for nilafishfarming cagesystems in physics, namely the temperature Stem water Sibakur eligible because the water temperature of all test samples are still within the range of 25-290C. Color and water requirements. (2) The water quality for fish rod Sikabur chemically meet requirements that included pH, Carbohydrate (CO2) to meet the requirements of the upstream and downstream while the center does not meet the requirements, Dissolved oxygen (DO), phosphate (PO4), and Ammonia ( NH3) does not meet the requirements due to exceeding quality standards for tilapia farming.
DAMPAK EROSI TEBING SUNGAI (STREAMBANK EROSION) TERHADAP PERUBAHAN PENGGUNAAN LAHAN PINGGIR BATANG BANGKO DI KABUPATEN SOLOK SELATAN Agustian, Dani; Edial, Helfia; Zuriyani, Elvi
Pendidikan Geografi Vol 2, No 1 (2013): Jurnal Mahasiswa Prodi Pendidikan Geografi
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This study aims to analyze, collect, and process and describe the changes in river flow conditions caused by: 1) the condition of land use change caused by erosion of the river banks around the edge of the Batang Bangko, 2) the condition of river bank erosion caused by the river around the edge of the cliff rod Batang Bangko, 3) the speed of the river flow due to changes in land and river bank erosion 4) changes in stream flow direction Batang Bangko streambank erosion. This study uses a descriptive method that aims to explain, a portrait of the symptoms, the facts and the nature of the research area. The results showed that: 1) changes occur throughout Nagari land traversed by the Batang Bangko lengths vary between 87 m - 121 m. Changing land is paddy fields into streams. The main causes of land use change is the streambankerosion, 2) conditions along in general Bangko Batang is the streambanks. Streambank erosion caused by human activities in managing and treating nature.Activities Class C mining (sand and gravel) exploit many rivers and the surrounding areas, so that the carrying capacity of the streambank to decline, 3) Speed at Batang Bangko found diverse, thereby potentially streambank erosion along stream Batang Bangko. Average flow rate obtained at all points of observation ranged from 2.07 to 2.69 m / sec. As a result, the speed of the flow can also affect the river bank erosion in streams and Batang Bangko 4) Changes in flow direction of the river occurs at each sample point through which the Batang Bangko is also changing the varying distances 18-28 m and occurs in the left and the right of the river. Streams left turn into scrubland. The main causes of changes in flow direction of the flow is caused by human activity and the speed of the flow and the absence of vegetation land cover found on the riverbank.
ANALISIS POTENSI AIR TANAH DANGKAL UNTUK KEBUTUHAN MASYARAKAT DI PADANG ARO KABUPATEN SOLOK SELATAN Widyawati, Siska; Edial, Helfia; Farida, Farida
Pendidikan Geografi Vol 2, No 2 (2013): Jurnal Wisuda Ke 47, Pendidikan Geografi
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The uncreasing of clean water specially for drinking purpose become a major issue in a lot place in Ind. The good quality and quantity of water are the basic need for the community. This study was conducted to analized the potential for ground water and likely to be developed in order to support the water needs in the city of Padang Aro.This study classified as descriptive research, to illustrate the potential of shallow ground water in the city of Padang Aro in quality (physical, chemical, and biological) as well as the quantity (shallow ground water discharge and water needs for the community) to meet the needs of people living in city of Padang Aro.The results showed that the physical quality of shallow ground water to meet water quality predetermined of Menteri Kesehatan RI. No. 492/MENKES/Per/IV/2010, chemical quality of shallow ground water does not meet the water quality requirements established Ministry of Menteri Kesehatan RI. No. 492/MENKES/Per/IV/2010 and if viewed in terms of the biological quality of shallow ground water does not meet the water quality requirements established of Menteri Kesehatan RI. No. 492/MENKES/Per/IV/2010. Shallow groundwater discharge in Padang Aro relatively very small because the range between 0.061 to 0.013 m3/second m3/second. 60.29% people of Padang Aro using shallow ground water for their daily needs. Where shallow ground water requirement per family ± 404.88 liters / family / day and needs of individuals ± 99.27 liters / person / day. If all residents of Padang Aro using shallow ground water for their lives, then the amount of water needs community as a whole paddock aro ± 1,289,943.9 liters / day. Shallow groundwater discharge contained in Padang Aro daily average is 7551.36 L / day, while the average water requirement per day per family is ± 404.88 liters / family / day, so it can be interpreted that the shallow groundwater in Padang Aro able to meet the water needs of the people in Padang Aro.
PERUBAHAN POLA CURAH HUJAN DI KECAMATAN KOTO XI TARUSAN KABUPATEN PESISIR SELATAN (TAHUN 2003 - 2012) Yani, Zulhijah Defitri; Edial, Helfia; Farida, Farida
Pendidikan Geografi Vol 2, No 2 (2013): Jurnal Wisuda Ke 47, Pendidikan Geografi
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The research was based on a different pattern of rainfall in the Distric t XI Tarusan Koto. The result of  this study reveals the magnitude of the average rainfall that occurred in District XI Tarusan Koto in the period 2003-2012 as well as changes in rainfall patterns.This  research  used  descriptive  quantitative  method  for  processing  of  secondary  data. Quantitative descriptive research is to conduct secondary data description of the data and then perform  data  analysis  to  obtain  conclusions.  This  research  area  is  Koto  XI  Tarusan,  South Coastal  District.  The  research  data  was  taken  from  the  station  BMKG  Regional  Sicincin  and PSDA West Sumatra province. Of all the data taken on average  of 10 years  from 2003 to 2012 from  of  three  point  of  observation  post  located  in  Koto  XI  Tarusan,  Nanggalo  Tarusan,  and Duku.The  results  showed  that  :  1)  The  average  rainfall  in  the  2003-2012  observation  period ranged  from  2749.3  to  3136.3  mm  /  year  and  (2)  the  rainfall  in  the  sub  District  Tarusan, equatorial rainfall  pattern obtained with bimodal shape ( two peak rainfall  ), where low rainfall occurred  in  January-June,  while  the  high  rainfall  occurred  in  August-December.  Of  the  three rainfall stations, there are no changes in rainfall patterns mean.
STUDI MINERAL AIA TIGO RASO (AIR TIGA RASA) UNTUK AIR MINUM DI NAGARI TANJUNG SANI KECAMATAN TANJUNG RAYA KABUPATEN AGAM Sartika, Meri Dewi; Edial, Helfia; Zahara, Leni
Pendidikan Geografi Vol 2, No 1 (2013): Jurnal Mahasiswa Prodi Pendidikan Geografi
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The water is clean and healthy has to be a standard in which the consumption point is to avoid the introduction of disease from bacteria or other substances into the body that will be harmful to health. Water from Tigo Aia Raso in trust by the public has properties to cure diseases. In order to prove the efficacy of the public is willing to consume water and Aia Three Raso although quality testing as well as the minerals contained in it has never been done before. The study was descriptive using qualitative methods. To view the mineral content in Aia Raso Tigo (Three Water Sense) is pH, Fe, Na and H2S. Water in thoroughly immediately put into sterile bottles and brought to the Analytical Laboratory. The study found content of pH on the inside of the water source the Aia Tigo Raso is at 6.27 and the outside source of water is equal to 6.18. The content of iron (Fe) on the outside of the water is equal to 3.27 mg / l and to the inside of the water is 3.95 mg / l. Mineral content of Sodium (Na) on the outside of the water is equal to 107.43 mg / l and the inside of the water is equal to 106.72 mg / l. Content of Sulfide (H2S) on the outside and the water source is a small note of <0.001 mg / l.
STUDI TINGKAT BAHAYA EROSI BERDASARKAN PENGGUNAAN LAHAN PADA SATUAN BENTUK LAHAN VULKANIK DI JALAN SIMPANG AMPEK–TALU KECAMATAN TALAMAU KABUPATEN PASAMAN BARAT Susilawati, Susilawati; Edial, Helfia; Farida, Farida
Pendidikan Geografi Vol 2, No 2 (2013): Jurnal Wisuda Ke 47, Pendidikan Geografi
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This research was conducted with the aim of ; 1) Determine the level of erosion hazard based on slope unit of land form unit in Jalan Simpang Ampek – Talu Talamau District, 2) Knowing the rate of erosion on the density of the vegetation cover unit of land based unit of land form in the Jalan Simpang Ampek – Talu Talamau District, 3) Knowing the rate of erosion rainfall based on land form unit in Jalan Simpang Ampek – Talu Talamau District, 4) Knowing the rate of erosion on the use of land based on land form unit in Jalan Simpang Ampek – Talu Talamau District. Existing units of land in the study area consists of land 48 land units and samples were taken only 4 units of land.Techniq to take sample with purposive sampling manner deliberately, the researchers determine their own samples taken based on the certain considerations. This study classified as descriptive research. Descriptive research is a research procedure that uses descriptive data in the form of words written or spoken of the people and actors that can be observed. The research focus on the actual problems that have happened and what the data is desired without manipulated.The results showed that the rate of erosion differ based on the use of land in the units of land on volcanic hills (V3) ; 1) The potential erosion contained in the class II midle category where the risk of erosion are there, but rarely found in sample 1 V3.III.Pm.Tmv.Lat driving factor is the slope of erosion and precipitation and sample 2 at V3.III.Sw.Tmv.Lat driving factor is the rainfall erosion, 2) Of potential erosion class III contained in the high category where the risk of high attrition, erosion often found in sample 3 at V3.III.Kc.Tmv.Lat is the driving factor of slope erosion, vegetation density land cover and rainfall and sample 4 at V3.III.Ht.Tmv.Lat is the driving factor of slope erosion, vegetation density land cover and rainfall.           
Co-Authors A.A. Ketut Agung Cahyawan W ahyuni . Anak Agung Istri Sri Wiadnyani Aprizon Putra Ardian Syahroni asef tionanda Aslan Sari M.Si SP. Thesiwati Aslan Sari Thesiwati BONI ashari Cici Gusnia Risyanti Cici Yulianti Dani Agustian Deded Chandra Dedi Hermon Devira Frissilla Milton Diah Permata Sari DINO WILMANSYAH Dwi Cahyo Kurniawan Elva Gamiarsih Elvi Zuriyani Endah Purwaningsih Erna M.Si Juita S.Pd Fajar Tamril Farida Farid Farida M.Sc. S.Si Febby Fitri Yolanda Febri Hasanta Febri Satrianto febriandi . ghinna rahmatania Hakiki Mulyani Harimanando Harimanando Helga Oktaviana Hera Nopianti Hilda Yetri Intan dwi rahayu IRFAN JUSAR Lafzia Tri Mahzuro Lailatur Rahmi Lara Odia Apriyanti Leni Zahara Lia Junita Mahesa Ragil Syofyan Meri Dewi Sartika Mimi Yulia Putri N Nofrion naufal zikry arrahman Nova, Sari Novio, Rery Nur Azimah YY nurkholilah nurkholilah Putri, Sri Kandi Rahmawati Ulfa Rahmi Zulva Rahmi Zulva, Rahmi Ratna Wati Ratna Willis Rauda tul Husna Resma Yani Ressa Andriani rexy elnando riang wirastin harefa Rina Febri Yani Astuti Ristalia Ristalia Rizki Putra Rozana M.Si Eka Putri Sepka Marnil Siska Siska Siska Siska Siska Widyawati sisva yetty Softi Nur Rahmah Sonia Sonia Sri Mariya Sriwinda 22 12 Suci Allara Putri Sutria Desman Tessa Melinda TITI INDRAYATI Triyatno . Triyatno . Triyatno Triyatno veni Nopriyanti VINA SEFIANI Vir Diannisa Zhra Welia Putri Widya Meisya Hardin Widya Prarikeslan Yoga Rahmata Yudi Antomi Yuherman Yuherman Yulia Armi Pitri Zulhijah Defitri Yani