Pengetahuan Siswa Mts Muhammadiyah Tawangsari Dalam Kesiapsiagaan Bencana Gempa Bumi Di Kabupaten Sukoharjo

Penelitian ini bertujuan untuk mengetahui pengetahuan dan kesiapsiagaan siswa dalam menghadapi bencana gempa bumi di MTs Muhammadiyah Tawangsari Kabupaten Sukoharjo. Penelitian ini merupakan jenis penelitian deskriptif kuantitatif dengan menggunakan perhitungan presentase untuk mengetahui pengetahuan dan kesiapsiagaan siswa dalam menghadapi bencana gempa bumi. Teknik pengambilan sampel dengan menggunakan teknik simple random sampling yaitu teknik pengambilan sampel secara undian (acak). Populasi siswa MTs Muhammadiyah Tawangsari adalah 171 siswa dan jumlah sampel yang diambil dalam penelitian ini adalah 108 siswa dari kelas VIIA, VIIB, VIIC, VIIIA, VIIIB, IXA, dan IXB yang ada pada tabel penentuan jumlah sampel dari populasi dengan taraf ksalahan 10% (Sugiono, 2010). Pengumpulan data pada penelitian ini dengan menggunakan angeket/kuesioner yang harus diisi oleh responden yang telah ditetapkan oleh undian. Hasil penelitian menunjukkan bahwa untuk pengetahuan siswa kelas VII terhadap bencana gempa bumi cenderung baik. Pengetahuan siswa kelas VIII terhadap bencana gempa bumi cenderung baik. Pengetahuan siswa kelas IX terhadap bencana gempa bumi cenderung baik. Sedangkan untuk hasil kesiapsiagaan siswa kelas VII dalammenghadapi bencana gempa bumi memiliki indeks 46,42 termasuk dalam kategori ikurang siap. Kesiapsiagaan siswa VIII dalam menghadapi bencana gempa bum memiliki indeks 48,48 termasuk dalam ketegori kurang siap. Kesiapsiagaan siswa IX dalam menghadapi bencana gempa bumi memiliki indeks 61,97 termasuk dalam ketegori hampir siap

Pengetahuan Siswa Tentang Mitigasi Non Struktural Bencana Gempabumi SMK Muhammadiyah 01 Wedi Kabupaten Klaten

Tujuan peneitian ini ingin mengetahui pengetahuan siswa terkait bencana gempabumi dan mitigasi non structural dalam menghadapi bencana gempabumi yang dilakukan oleh siswa di SMK Muhammadiyah 01 Wedi Kecamatan Jogonalan Kabupaten Klaten. Subyek penelitian ini mencakup siswa yang berada di SMK Muhammadiyah 01 Wedi Kabupaten Klaten dan kondisi tata ruang yang berada di SMK Muhammadiyah 01 Wedi Kabupaten Klaten. Penelitian ini menggunakan pendekatan kualitatif dengan jenis deskriftif kualitatif yang merupakan metode penelitian yang datanya bukan angka-angka,melainkan berupa kata-kata, kalimat dan gambar melalui sumber data primer dan data sekunder dengan teknik pengambilan data melalui wawancara,angket, dan observasi. Teknik analisis data yang digunakan adalah model Miles and Huberman yang meliputi reduksi data, penyajian data, kesimpulan. Berdasarkan analisa data yang di peroleh pengetahuan siswa terhadap bencana gempabumi di SMK Muhammadiyah 1 Wedi Kabupaten Klaten diklasifikasikan baik dan tingkat pengetahuan siswa terhadap mitigasi non struktural SMK Muhammadiyah 1 Wedi Kabupaten Klaten di klasifikasikan baik siswa mampu memahami atau mengetahui sikap mengenai mitigasi non struktural (mengetahui cara menempatkan sarana prasarana atau infrastruktur yang tepat agar tidak membahayakan dan menimbulkan korban jiwa)

Evaluasi Ruang Terbuka Hijau di Kecamatan Kota Martapura Kabupaten Ogan Komering Ulu Timur Provinsi Sumatera Selatan

The current urban area in nowadays development has a lot of negative impacts occurring mainly on environmental aspects, such as the occurrence of abuse on available land. Any land use can affect the environment. One of them for green open space. Therefore, the research for the evaluation of green open spaces whether available and meets the standards of the Act. The method used in the research was conducted by survey method in Kecamatan Martapura. Technical implementation is done by data collection, and the selection of location observations is made purposively. The data have been analyzed descriptively. The results showed that Martapura District has green open approximately of 37.37% in the form of green open space of public and private green open space. As mentioned in the RI Act No.26 Year 2007 Kecamatan Martapura fullfils this criteria. The distribution of green open spaces in Kecamatan Martapura is almost adequately distributed in every village and kecamatan, although there are still some areas that do not have green open space yet

Kesiapsiagaan Siswa SMP N 3 Gantiwarno Kabupaten Klaten Dalam Menghadapi Bencana Gempa Bumi

Kecamatan Gantiwarno di Kabupaten Klaten adalah salah satu wilayah yang mengalami kerusakan cukup parah akibat genpa bumi yang terjadi 27 Mei 2006 dengan episentrum di selatan Yogyakarta. Sehingga di perlukan kesiapsiagaan untuk menghadapi bencana gempa bumi sebagaimana yang dilakukan di sekolah SMP N 3 Gantiwarno di Teluk, Kelurahan Kragilan, Kecamatan Gantiwarno, Kabupaten Klaten. Penelitian ini dilakukan di SMP N 3 Gantiwarno dengan judul “Kesiapsiagaan Siswa SMP N 3 Gantiwarno, Kabupaten Klaten Dalam Menghadapi Bencana Gempa Bumi”. Penelitian ini bertujuan (1) Mengetahui tingkat kesiapsiagaan siswa SMP 3 Gantiwarno, Kabupaten Klaten, dalam menghadapi bencana gempa bumi. (2) Mengetahui hubungan tingkat kelas terhadap kesiapsiagaan siswa SMP N 3 Gantiwarno dalam menghadapi bencana gempa bumi. Penelitian dilakukan dengan menggunakan pendekatan kuantitatif dengan metode diskriptif. Teknik pengumpulan data menggunakan teknik angket, teknik dokumentasi, dan teknik observasi. Teknik analis data yang di gunakan adalah tingkat indeks kesiapsiagaan dengan katagori sangat siap, siap, hampir siap, kurang siap, kurang siap, dan belum siap dan teknik chi square serta analisis korelasi . Hasil yang diperoleh dalam penelitian ini adalah (1) Tingkat kesiapsiagaan siswa SMP N 3 Gantiwarno, Kabupaten Klaten dalam menghadapi bencana gempa bumi termasuk dalam kategori kurang siap, dengan perolehan niali prosentase 52,99% (Skala 100). (2) Melalui analisis crostabs teknik chisquare diperoleh hasil tidak ada hubungan antara tingkat kelas dengan kesiapsiagaan, untuk mengetahui keabsahan antara kedua variabel yaitu tingkat kelas dengan kesiapsiagaan siswa maka dilakukan kembali uji dengan menggunakan korelasi spearman Rank hasil menunjukkan adanya hubungan positif yang sangat signifikan dari kedua variabel, masing-masing memiliki korelasi yang cukup kuat antara tingkat kelas dengan kesiapsiagaan siswa SMP N 3 Gantiwarno dalam menghadapi gempa bumi

Analisis Risiko Bencana Kekeringan di Kabupaten Klaten

This drought disaster risk research was conducted in Klaten Regency. The first purpose is to analyze the level of drought hazard, the level of vulnerability against drought and the level of capacity to face drought disaster in Klaten Regency. And the second purpose is to analyze the level of drought disaster risk in Klaten Regency. The method used is secondary data analysis which consist of combined quantitative and qualitative method. The data analysis technique uses quantitative GIS overlay and mathematical computing with classification and scoring of each parameters acording to weighted method to obtain the first research purpose. The second research purpose is obtained using qualitative method trough disaster risk matrix classification by overlaying the first results. The unit of drought risk analysis used here is land units. The results obtained show that the areas in Klaten Regency which have high risk level of drought disaster is covering 4.860,46 hectares (7%) and spread in most of districts in Bayat, Trucuk and Juwiring, and slightly in Gantiwarno and Karangdowo. Areas with moderate risk covering 21.521,02 hectares (31%) is spread in the district of Bayat, Trucuk, Juwiring, Gantiwarno, Karangdowo, Manisrenggo, Ngawen, Tulung, Pedan, Kemalang, Kalikotes, Cawas and Prambanan. While the remaining areas covering 43.641,84 hectares (62%) have low risk level of drought disaster

Analisis Pengaruh Perubahan Penggunaan Lahan Terhadap Debit Puncak Sub DAS Kali Premulung Tahun 2006 dan 2014

This research was conducted in Kali Premulung Watershed which is one part of Bengawan Solo Watershed. This study aims to determine how much land use change and its effect on the coefficient runoff and peak discharge in Kali Premulung Watershed at 2006 and 2014. The research method used is the method of secondary data analysis. Secondary data obtained from Government Institutions in the form of rainfall data from 5 stations within 10 years, also map of soil type, slope, river network and land use. The analysis used in the form of descriptive analysis on the spatial distribution pattern of land use and its effect on the runoff coefficient in 2006 and 2014. From the research results show that Kali Premulung Watershed has an average rainfall area of 101.84 mm in 2006 and 60.78 mm in 2014. Changes in land use that occurred between 2006 to 2014 ie water pool decreased as much as 0.13 km2, gardens increased as much as 0.22 km2, settlements increased by 6.63 km2, grass decreased by 0.73 km2, rice fields decreased by 5.38 km2, rocky ground increased by 0.17 km2 and mooring area decreased by 0.75 km2. From the scoring results using the Cook Method in 2006 the runoff coefficient of Kali Premulung Watershed has a coefficient of runoff of 42.75, while in 2014 has a runoff coefficient of 43.14. It shows that the effect of land use change on the increase of runoff coefficient. The results of the peak discharge calculation using rational method in 2006 with rainfall intensity of 7.08mm / hour provides a peak discharge value of 64.52 m3 / sec, while in 2014 with rainfall intensity of 5.05 mm / hour provides the value of the discharge peak of 46.38 m3 / sec. An increase in runoff coefficient of 0.39 affects the increase in peak discharge amounts of 0.71 m3 / s if the intensity of rainfall in each year is calculated based on the average rainfall intensity during the research period which is 7.76mm / hour. However, due to the tendency of direction of rainfall intensity trend that decreased from 2006 to 2014, causing the estimated amount of peak discharge decreased by 18.14 m3 / sec

Analisis Penggunaan Lahan Tahun 2013 terhadap Ketersediaan Air di Sub Daerah Aliran Sungai Blongkeng

Farmland drought that hit some areas at Blongkeng Sub Watershed in 2013 affect of the water balance. Potential of water supply at non-domestic landuse is affected by the water needs in each landuse patterns. Decreasing of land for uptake and catchment rainfall is one of the factors that affect water balance system. The purpose of this research 1) Estimated availability of water at Blongkeng Sub Watershed, 2) Knowing the water needs based on the pattern of land use in 2013 at Blongkeng Sub Watershed, and 3) Analyze the water balance by months of wet and dry season preformance scope of Sub Watershed assessment. The research method using Thronthwaite Matter water balance, data sources of hidrometereologi such as rainfall and temperature from 3 stations around Blongkeng Sub Watershed for 10 years (2004-2013). Water needs from pattern of land use obtained through data processing based Remote Sensing and Geographic Information System. Landsat 8 recording June 2013 is processed into maps of land use in 2013 Blongkeng Sub Watershed, conducted a survey with purposive sampling method. Size of each land use can be known from the calculation of water needs. The potential of water availability is a comparison between amount of water available requirements. Results of this research 1) Potential of water availability in each month is the lowest at rice field ranged from 6-180 mm3/year while the highest in each month is open land and lava – volcanic mudflow range between 6000-3900000 mm3/year, 2) The water needs is directly inversely with the water availability, the lowest requirement is open land with average 1000 mm3/year while the highest is a rice land with an average 4.5 to 12 million mm3/year, 3) Percentage value of the deficit / surplus each land use patterns in the wet season has surplus between other forest land, mix plantations, lava – volcanic mudflow, and open land while in the dry season has deficit at the land around settlements, rice field, and terrain/fields. Vulnerability to drought at Blongkeng Sub Watershed predicted occur in August – October. Keywords: Drought, Water Availability, Water Requirements, Thronthwaite Matter, Water Balanc

Peran Simulasi Bencana Terhadap Kesiapsiagaan Siswa Kelas VII Dalam Menghadapi Bencana Gempa Bumi Di MTs Negeri Gantiwarno Kecamatan Gantiwarno Kabupaten Klaten

Gempa bumi adalah suatu gejala fisik atau kejadian alam yang umumnya ditandai dengan bergetar/berguncangnya bumi. Penyebab gempa umi yang selama ini disepakati antara lain dari proses tektonik, akibat pergerakan kulit/lempeng bumi, aktivitas sesar di permukaan bumi, pergerakan geo-morfologi secara lokal (contoh: terjadinya rutuhan tanah), dan aktivitas gunung api serta ledakan nuklir. Tujuan penelitian ini untuk (1) mengetahui kesiapsiagaan siswa kelas VII sebelum diadakan simulasi bencana gempa bumi dan (2) mengetahui kesiapsiagaan siswa kelas VII setelah diadakan simulasi bencana gempa bumi. Penelitian ini menggunakan metode eksperimen, metode pengambilan data secara sampel, dengan jumlah sampe sebanyak 111 siswa dan teknik analisis data menggunakan deskriptif kuantitatif. Pengumpulan data menggunakan angket, wawancara, observasi, dan dokumentasi. Hasil penelitian diperoleh indeks gabungan kesiapsiagaan sebelum simulasi bencana sebesar 77,07 masuk kategori siap sedangkan indeks gabungan kesiapsiagaan sesudah simulasi bencana sebesar 86,39 masuk kategori sangat siap. Peningkatan terjadi pada sebelum simulasi dan sesudah simulasi. Sebelum simulasi masuk dalam kategori siap dan sesudah simulasi masuk kategori sangat siap

Analisis Hubungan Penutup Lahan Dengan Suhu Permukaan Lahan Menggunakan Penginderaan Jauh Di Kabupaten Klaten Tahun 2016

The growing problem of population growth in Klaten regency for each year and the increasing human need for land will encourage people to convert land from agricultural land to non-agricultural land. The change of land affects the change of surface temperature of the surrounding land. This study aims to: 1) map the land cover and surface temperature in Klaten District, 2) analyze the relationship between land cover and surface soil temperature. Results Land cover and surface temperature of the land are extracted from remote sensing imagery ie Landsat image by means of digital image processing. The method used is overlay analysis to produce overlay map of land cover and surface temperature of the land. Field observation was done by using purposive random sampling method. Observational factors such as land use, field temperature, vegetation type . The results of this study show the overlay data of land cover with surface temperature in 2016. The dominant land cover is 407 km ² (57.98%) agricultural land cover and the dominating surface temperature is the high temperature of 29-32 ° C. observation results showed very high temperatures were in the settlement cover of 34.1 ° C and very low temperatures were in the non-agricultural land cover 20.8 ° C. The temperature difference on the same land cover lies in the utilization of the land and the type of vegetation. There is a relationship between the land cover and the temperature of the land area indicated by the corresponding number of samples of 28 between the assumption results and the overlay result. Keywords: Land Cover, Land Surface Temperature, Remote Sensing, Image Processin

Estimasi Potensi Limpasan Permukaan dengan Menggunakan Data Penginderaan Jauh dan Sistem Informasi Geografi di Daerah Aliran Sungai Kayan Provinsi Kalimantan Utara

Land use transfer is one of the factors causing the change of hydrogi output in a watershed. Changes in land from non-built to built indicate that the area has the potential for floods to run up. This is because the low level of infiltration causes the surrounding soil to be impermeable to water, especially in the soil texture which has clay texture. This area is often found in downstream areas, especially in the Tanjung Selor watershed. This study aims to: determine the level of remote sensing data accuracy in estimating the potential for surface runoff and analyze the surface runoff coefficient in each sub watershed and the distribution of potential surface runoff in the Kayan watershed. The research method used in knowing the surface runoff coefficient in each sub watershed is by using the cook method. This method uses slope, drainage density and infiltration variables obtained from processing DEM SRTM 90 M and land use variables obtained from the interpretation of Spot Spot 7 in 2016. The use of this method aims to obtain coefficient values in each watershed. The greater the surface runoff coefficient, the greater the potential for flood runoff. The results obtained from the calculation of accuracy test in knowing the level of accuracy of remote sensing data to estimate the potential for surface runoff that is equal to 73.33%. That is, the data is suitable for future research. The influence of the coefficient value in estimating the potential for surface runoff is obtained by the value which has the largest number of coefficients in the Tanjung Selor watershed which is around 55.73%. The magnitude of the coefficient value in the area is influenced by the relatively flat slope of the slope to cause the coefficient to be greater, namely 25.74. The higher the coefficient value generated, the greater the potential for surface runoff