dc.contributor.author | Anna, Alif Noor | |
dc.contributor.author | Kaeksi, Retno Woro | |
dc.contributor.author | Astuti, Wahyuni Apri | |
dc.date.accessioned | 2012-03-19T05:18:56Z | |
dc.date.available | 2012-03-19T05:18:56Z | |
dc.date.issued | 2010-07 | |
dc.identifier.citation | Anna, A.N., et al (2006) Analisis Karakteristik Parameter Hidrologi Akibat Alih Fungsi Lahan di Daerah Sukoharjo Melalui Citra Landsat Tahun 1997 dengan Tahun 2002. Surakarta: Fakultas Geografi UMS. Anna, A. N. (2001) Agihan Kualitas Air Tanah Daerah Perkembangan Kota Antara Surakarta – Kartasura. Forum Geografi. vol. 15, no. 1, Juli. Arpan. F., Galuh, C.K.D., dan Sudjarwadi (2004) Kajian Meteorologis Hubungan Abtara Hujan Harian Dan Unsur-unsur Cuaca: Studi Kasus di Stasiun Meteorologi Adisucipto Jogjakarta. Majalah Geografi Indonesia, vol. 18, no. 2, September. Hadi, M.P. dan Endarmiyati (1999) Model Perhitungan Indeks Kekritisan Air, Studi Kasus DAS Kreo. Geosfer, vol. 1, Oktober. Muhsinatun (2000) ‘Defisit Air Jawa-Madura Sangat Serius’. Solopos, 23 Maret. Pemerintah Kabupaten Sukoharjo (2000) Neraca Sumberdaya Alam Daerah Kabupaten Sukoharjo Tahun 1999. Sukoharjo: Bappeda Danoedoro, P. (1996) Pengolahan Citra Digital Teori dan Aplikasinya Dalam Bidang Penginderaan Jauh.Diktat Kuliah. Yogjakarta:Fakultas Geografi UGM. Laviani, R., et al (2003) Pengaruh Kondisi Sosial Ekonomi Penduduk dan Perubahan Jenis Penggunaan Lahan Terhadap Limpasan Di DAS Bodri Kendal Jawa Tengah. Forum Geografi, vol. 17, no. 1, Juli. Nugroho, S. (2006) Penggunaan Citra Landsat untuk Mengetahui Perubahan Penggunaan Lahan Di Sebagian Wilayah Subosuka. Skripsi. Surakarta:Fakultas Geografi UMS Soetikno. 1989. Studi Geomorfologi untuk Evaluasi Sistem Penyediaan Air Bersih di DAS Serang Kulon Progo. Yogjakarta: Fakultas Geografi UGM. Suyono. 1995. Pengelolaan Sumberdaya Air. Jogjakarta: Fakultas Geografi UGM. Suyono. 1996. Pengelolaan Daerah Aliran Sumngai Dalam Konteks Hidrologi Dan Kaitannya Dengan Pembangunan Berkelanjutan. Pidato Pengukuhan Jabatan Lektor Kepala Madya Pada Fakultas Geografi UGM. Jogjakarta: Fakultas Geografi UGM. Murtiono, U.H., et al (2001). Studi Karakteristik Hujan Dan Regim Sungai DAS. Laporan Penelitian. Surakarta: Balai Teknologi Pengelolaan DAS Departemen Kehutanan. | en_US |
dc.identifier.issn | 0852-0682 | |
dc.identifier.uri | http://hdl.handle.net/11617/575 | |
dc.description.abstract | The Study, carried out Sukoharjo, deals with the effect of land function change from 1997 to 2002
toward the change of chosen hydrological parameters. The hydrological parameter constituses the coefficient
runoff (C), the extra soil water (id), and the amount of constant stream (Wa). The process of land
function the change is searched by using landsat image composit RGB (Red Green Blue) 452. Meanwhile,
the aims of the study are (1) to determine the types and distribution for the process of land function
change, and (2) to analyze the change of coefficient value runoff (C), the extra soil water (Id), and the
amount of constant stream (Wa) within the area of research. The result of the study shown that there are
many types of land function change, which occurred in almost all the area of research except the one type
coming from the river becoming wet/dry rice field/residence/forest of which only occurred in Nguter sub
district. The condition because of the straightening Bengawan Solo River in the sub district, cousequenly,
the land function change proceses from the river into the land and vice versa. Moreover, of the 7 types of
land function change in the area of research, the widest type of land function change covering the whole
district is a change from forest/ horticulture/dry or wet rice field into residence. The effect of such a change
has also caused a change in the characteristics of chosen hydrological parameter. Such a change can be seen
from the value C, Id, and Wa. Furthermore, the change can be clarified as follow: the value C and Wa
tend to rise while Id tends to decrease. This mean that the land function change has resulted in great
abundant and decrease of water absorbed in the soil. In general, the availability of water source within
the area can still be supplied from the seemingly increased constant stream. Such a condition might be
caused by the ratio between the built land and the proportional open land of which about > 30 % of the
whole space. | en_US |
dc.subject | land fuction change | en_US |
dc.subject | hydrology parameter | en_US |
dc.subject | coefficient runoff | en_US |
dc.subject | the extra soil water | en_US |
dc.subject | the amount of constant stream | en_US |
dc.title | ANALISIS KARAKTERISTIK PARAMETER HIDROLOGI AKIBAT ALIH FUNGSI LAHAN DI DAERAH SUKOHARJO MELALUI CITRA LANDSAT TAHUN 1997 DENGAN TAHUN 2002 | en_US |
dc.title.alternative | The Analysis of Hidrological Characteristics Parameter as The Effect of Landuse Changing Using Landsat Image From 1997 to 2002 in Sukoharjo District | en_US |
dc.type | Article | en_US |