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Analysis of Groundwater Advance Decline in Surakarta City Cholil, Munawar
Forum Geografi Vol 12, No 2 (1998)
Publisher : Forum Geografi

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This research was intended to know the cause of a drawdown of artesian groundwater surface and analyze on exploiting its groundwater in Surakarta. The total amount of groundwater exploitation in Surakarta will be 69,206.4 m3Â if it is compared the groundwater runoff capacity of unconfined aquifer as with 8,860.9 m3 a day and confined aquifer as 42,447.3 m3 a day. Thus, the total amount of groundwater runoff in Surakarta is 51,308.2 m3 a day. Groundwater exploitation has exceeded the capacity of groundwater runoff as 17,898.2 m3, so the reservoir of groundwater is going to reduce continually. Groundwater exploitation in the loation of the researh has caused a piezometric drawdown. In 1990, its piezometric was negative, it means that the position of the piezometric was under the surface of land, while in 1990Â artesian well indicated that its piezometric was almost nearly positive. Thus, the piezometric drawdown average 9.4 m3. In the center of the ity, it happened the cone of depression at piezometric contour in 1990, so a piezometric drawdown that resulted from groundwater exploitation exceeding the runoff of groundwater was proved. As a result of groundwater exploitation excessively, it resulted in the inequilibrium of groundwater. This depession has been extending continually as a result of adding wells, so it result in a groundwater drawdown permanently, as happened in the location of the research.

Groundwater Quality and the Settlements Condition in Cholil, Munawar
Forum Geografi Vol 10, No 1 (1996)
Publisher : Forum Geografi

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To comprehend the factors which influence on the juvenile water, it needs paying attention to the rocks permeability, the thickness of the aeration zone, the type of the material composition and the depth of the ground water. The grade of the ground water quality, both ground water in general and juvenile water in the urban, is dependent upon the natural physical, man made physical, and the condition of the local inhabitant besides the another factors. The influence grade of the factors are undersirable yet because among of them there are cross-linkages. The linkage of the ground water quality condition, besides another factor, inconfirmed by the inhabitant and the settelement. The aspect of the man made physical, both sanitation condition and the population density with their activity effect i.e. sewage by product, should fully determine the ground water quality. There is a closed connection between the juvenile water quality and the settlement condition, mainly, in the case is the domestic sewage disposal. It is estimated that the unit of settlement associates with the grade of the juvenile water quality. Some of the variabilities which are desirable to sustain the settlement condition and constitutes the influence variability i.e. the density of the population and buildings, and the condition of the drainage system for sewage.

Unconfined Groundwater Quality based on the Settlement Unit in Surakarta City Cholil, Munawar
Forum Geografi Vol 11, No 1 (1997)
Publisher : Forum Geografi

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The quality of groundwater of unonfined aquifer with growing population density is endangered by population. This may cause serious problem as greatest portion of the population utility groundwater of unconfined aquifer as their drinking water. This research is aim at studying the difference in quality of groundwater of unonfined aquifer in Surakarta Munipicality by settlement units, and studying the impact settlement factors and groundwater depth on the quality of groundwater of unonfined aquifer. The research was executed by a survey methhod, taking 44 units of groundwater of unonfined aquifer samples at stratified proportional random from 44 villages. The samples were analyzed at the laboratory of Local Drinking Water Company (PDAM) of Surakarta. Data were analyzed using by stiff diagram, variance analysis, and multiple regression. The research reveals that there is very little differences in the quality of free groundwater in Surakarta, as it is shown by same chemical properties. Several chemical properties were found very high in concentration, but the rest were simultaniously low. On the basis of minimum quality of drinking water coli content have exeeded the allowed limit for drinking water.Among the settlement units observed, there were no significant differences in the physical, chemical (except pH), bacteriological factors. This means that differences among various depth of water. Electrical onductivity (EC), Na, Mg, H2CO3, H2SO4, and NH3 were found different among various depth of water table. Major chemical conentration were significant with geology formation. Population density, built up areas, size of settlement, building density, and the condition of drainage simultaniously affect the quality of free ground water. No differences among settlement units was observed the most important fators determining the free groundwater quality was population density.

Analysis of Groundwater Advance Decline in Surakarta City Cholil, Munawar
Forum Geografi Vol 12, No 2 (1998)
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/forgeo.v12i2.470

This research was intended to know the cause of a drawdown of artesian groundwater surface and analyze on exploiting its groundwater in Surakarta. The total amount of groundwater exploitation in Surakarta will be 69,206.4 m3Â if it is compared the groundwater runoff capacity of unconfined aquifer as with 8,860.9 m3 a day and confined aquifer as 42,447.3 m3 a day. Thus, the total amount of groundwater runoff in Surakarta is 51,308.2 m3 a day. Groundwater exploitation has exceeded the capacity of groundwater runoff as 17,898.2 m3, so the reservoir of groundwater is going to reduce continually. Groundwater exploitation in the loation of the researh has caused a piezometric drawdown. In 1990, its piezometric was negative, it means that the position of the piezometric was under the surface of land, while in 1990Â artesian well indicated that its piezometric was almost nearly positive. Thus, the piezometric drawdown average 9.4 m3. In the center of the ity, it happened the cone of depression at piezometric contour in 1990, so a piezometric drawdown that resulted from groundwater exploitation exceeding the runoff of groundwater was proved. As a result of groundwater exploitation excessively, it resulted in the inequilibrium of groundwater. This depession has been extending continually as a result of adding wells, so it result in a groundwater drawdown permanently, as happened in the location of the research.

Groundwater Quality and the Settlements Condition in Cholil, Munawar
Forum Geografi Vol 10, No 1 (1996)
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/forgeo.v10i1.512

To comprehend the factors which influence on the juvenile water, it needs paying attention to the rocks permeability, the thickness of the aeration zone, the type of the material composition and the depth of the ground water. The grade of the ground water quality, both ground water in general and juvenile water in the urban, is dependent upon the natural physical, man made physical, and the condition of the local inhabitant besides the another factors. The influence grade of the factors are undersirable yet because among of them there are cross-linkages. The linkage of the ground water quality condition, besides another factor, inconfirmed by the inhabitant and the settelement. The aspect of the man made physical, both sanitation condition and the population density with their activity effect i.e. sewage by product, should fully determine the ground water quality. There is a closed connection between the juvenile water quality and the settlement condition, mainly, in the case is the domestic sewage disposal. It is estimated that the unit of settlement associates with the grade of the juvenile water quality. Some of the variabilities which are desirable to sustain the settlement condition and constitutes the influence variability i.e. the density of the population and buildings, and the condition of the drainage system for sewage.

Management of an Underground River to Overcome Water Scarcity in the Gunung Sewu Karst Area, Indonesia Amin, Choirul; Priyono, Priyono; Jauhari, Arif; Priyana, Yuli; Priyono, Kuswaji Dwi; Cholil, Munawar
Forum Geografi Vol 31, No 1 (2017): July 2017
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/forgeo.v31i1.4502

Since people living in a karst area periodically face a crisis due to a lack of fresh water, it is necessary to re-evaluate the ability to use water resources. An appropriate and effective management is required to use available water resource sustainably. We describe a management process of exploring underground river in karst region as water resources. The activities completed included four phases, namely exploration, pre-lifting activities, the water lifting and post-lifting activities. The exploration phase included speleological surveys and data collection for the cave mouth using remote sensing instrument. The pre-lifting was done to prepare various requirements before the lifting process was completed. The water lifting phase consisted of the construction of an underground river dam, the installation of submersible pumps, the construction of reservoirs and the installation of piping to connect to the public hydrant. The post-lifting phase was mainly conducted to organise water distribution evenly. This management model was evidenced to successfully overcome drought in Pucung village by providing fresh water to the local community. Moreover, this model promoted residentsâ cost savings by reducing their expenses for buying water from IDR 50,000/m3 to IDR 3,500/m3 (1,300 percent).

Unconfined Groundwater Quality based on the Settlement Unit in Surakarta City Cholil, Munawar
Forum Geografi Vol 11, No 1 (1997)
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/forgeo.v11i1.495

The quality of groundwater of unonfined aquifer with growing population density is endangered by population. This may cause serious problem as greatest portion of the population utility groundwater of unconfined aquifer as their drinking water. This research is aim at studying the difference in quality of groundwater of unonfined aquifer in Surakarta Munipicality by settlement units, and studying the impact settlement factors and groundwater depth on the quality of groundwater of unonfined aquifer. The research was executed by a survey methhod, taking 44 units of groundwater of unonfined aquifer samples at stratified proportional random from 44 villages. The samples were analyzed at the laboratory of Local Drinking Water Company (PDAM) of Surakarta. Data were analyzed using by stiff diagram, variance analysis, and multiple regression. The research reveals that there is very little differences in the quality of free groundwater in Surakarta, as it is shown by same chemical properties. Several chemical properties were found very high in concentration, but the rest were simultaniously low. On the basis of minimum quality of drinking water coli content have exeeded the allowed limit for drinking water.Among the settlement units observed, there were no significant differences in the physical, chemical (except pH), bacteriological factors. This means that differences among various depth of water. Electrical onductivity (EC), Na, Mg, H2CO3, H2SO4, and NH3 were found different among various depth of water table. Major chemical conentration were significant with geology formation. Population density, built up areas, size of settlement, building density, and the condition of drainage simultaniously affect the quality of free ground water. No differences among settlement units was observed the most important fators determining the free groundwater quality was population density.

Analisis Fluktuasi Hujan dan Morfologi Sungai terhadap Konsentrasi Banjir Daerah Surakarta Anna, Alif Noor; Suharjo, S; Cholil, Munawar
Forum Geografi Vol 25, No 1 (2011): July 2011
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/forgeo.v25i1.5033

This research aims to analyse rain fluctuation and river morphology to flood concentration in Bengawan Solo River, Surakarta. The method of this research is field survey supported by secondary data analysis. The survey was conducted using GPS (Global Positioning System). The result indicates that high intensity rainfall in the research area happened during October till April. River flow in dry season generally decreased in accordance with the distribution of low rainfall (dry month). Whereas, river flow rates seen to increase along with the rainfall that occurs in the rainy season. Other result show that point 11-18 (location in Tanjung village district of Sukoharjo till Semanggi village district of Pasar Kliwon) very superficial which became impact of the river. The point represent floods concentration, therefore if there is rain with high quantity, the water will rise and overflow to surface, especially point 11, 13, and 16 (Tanjung, Kedunggudel, and Telukan village district of Sukoharjo). The processes that occurred at these sites are sedimentation, and lateral erosion (horizontal erosion).

PENDIDIKAN DAN PELATIHAN SISTEM INFORMASI GEOGRAFI UNTUK ANGGOTA MUSYAWARAH GURU MATA PELAJARAN GEOGRAFI DI KABUPATEN SUKOHARJO DAN KABUPATEN SRAGEN PROPINSI JAWA TENGAH Cholil, Munawar; Priyono, Priyono; Hardjono, Imam
GERVASI: Jurnal Pengabdian kepada Masyarakat Vol 3, No 2 (2019): GERVASI: Jurnal Pengabdian Kepada Masyarakat
Publisher : LPPM IKIP PGRI Pontianak

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31571/gervasi.v3i2.1317

Keberhasilan pembelajaran banyak dipengaruhi oleh kemampuan guru. Artinya, di pundak gurulah keberhasilan pembelajaran dibebankan. Sementara realitas yang ada dan terjadi di lapangan, ada kesan bahwa kemampuan guru masih rendah. Sebagian besar dari mereka masih berpredikat sebagai pelaksana kurikulum, bahkan diantara kegiatan-kegiatan yang mereka lakukan lebih bersifat rutinitas. Guru belum siap menghadapi berbagai perubahan, di samping terbatasnya akses pada materi pembelajaran mutakhir. Motivasi dan kesiapan belajar peserta didik juga rendah. Kurangnya waktu belajar, lingkup materi yang sangat luas, serta laju/akselerasi perubahan (change) di bidang ilmu, teknologi dan seni berjalan begitu cepat. Mata pelajaran geografi mulai tahun ajaran 2008/2009 adalah salah satu materi ujian nasional, sehingga diperlukan peningkatan kualitas guru geografi untuk menunjang proses pembelajarannya. Pendidikan dan pelatihan SIG di kalangan guru-guru yang tergabung dalam Musyawarah Guru Mata Pelajaran(MGMP) Geografi, dengan peragaan dan praktek dibarengi simulasi GIS diharapan akan dapat memperlancar dan mempermudah proses pembelajaran geografi khususnya SIG. Bahwa melalui media pendidikan dan keterampilan SIG akan dapat terjalin kerja sama yang erat antara Fakultas Geografi dengan stake holder (sumber input mahasiswa baru) dengan harapan akan semakin meningkatkan minat belajar ilmu geografi di kalangan masyarakat, khususnya kepada peserta didik atau siswa-siswa smu tempat guru anggota MGMP Geografi tersebut bekerja . Hasil kegiatan ini adalah peserta Guru-guru Geografi mampu membuat peta tematik yang merepresentasikan wilayahnya yaitu Kabupaten Karanganyar dan Kabupaten Sragen. Luaran peta tematik dalam bentuk hardcopy dan softcopy.

ANALISIS MORFOLOGI DAN MORFOSTRUKTUR SERTA PENGARUHNYA TERHADAP BANJIR LUAPAN SUNGAI BENGAWAN SOLO HULU TENGAH Suharjo -; Alif Noor Anna; Munawar Cholil; Rudiyanto -
PROSIDING SEMINAR NASIONAL & INTERNASIONAL 2015: Prosiding Bidang MIPA dan Kesehatan The 2nd University Research Colloquium
Publisher : Universitas Muhammadiyah Semarang

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Bengawan Solo river flow changes is estimated to occur about 2 or at least a million years ago. The image interpretation results obtained ancient Bengawan Solo river which has become a valley winding naturally potential to be flood-prone areas. The aim of this study is to asses the condition of morphology and morphostructure of River Bengawan Solo and the impact towards flood overflow. This research use survey method. Data analyzed by quantitative descriptive technique, assisted with GIS analysis. The results of this study are (a) the morphology of the present; positive skewed figures means that the material is the result of fluvial processes and susceptible to flood overflow. The direction of the flow is toward the North, to the North Coast of Java which is lower, (b) morphostructure at the present; Solo River water level leads to the North, but at a certain point, there are seen places which are uphill or places which are higher than before, which are must lower for a uphill or a higher place than before, which are should be lower. This cause the tilt to rise. Silting and erosion occurs at a certain point. Point 11-18 are the point that be the impact of streamlining river, so its flow getting swift. At some point (between 11-18) it seem very close the distance between the water height and the ground level, means that the water height close to the height of the surface, so that leaving it vulnerable to flood overflow. This condition is particularly worrying in case of rain with a large quantity of water that will be up and overflow onto the surface. At point 11, 13, and 16 clear to see that the river is very shallow if it is compared to other points.Keywords: morphology, morphostructure, Flood Overflow, Watersheed

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