Hartono Hartono
Fakultas Geografi Universitas Gadjah Mada, Jl. Kaliurang, Bulaksumur, Yogyakarta 55281.

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FAKTOR-FAKTOR PENENTU KEKRITISAN DAN PENGEMBANGAN KRITERIA INDIKATOR KEKRITISAN EKOSISTEM GAMBUT TROPIKA DI TRUMON DAN SINGKIL PROVINSI ACEH (Determinant Factors of Criticality and Development Criteria Indicators for Critical Tropical Peat Ecosystem in Tr Aswandi Aswandi; Ronggo Sadono; Haryono Supriyo; Hartono Hartono
Jurnal Manusia dan Lingkungan Vol 22, No 3 (2015): November
Publisher : Pusat Studi Lingkungan Hidup Universitas Gadjah Mada

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.22146/jml.18757

Abstract

ABSTRAKHutan rawa gambut merupakan salah satu ekosistem spesifik dan kompleks. Terbatasnya pemahaman terhadap karakteristik biofisik dan sifat kritisnya menjadi akar masalah degradasi ekosistem gambut di Indonesia. Generalisasi penerapan kriteria lahan kritis menyebabkan penilaian menjadi tidak tepat, sehingga program rehabilitasi menjadi tidak efektif. Tujuan penelitian adalah menentukan faktor-faktor biofisik yang mempengaruhi tingkat kekritisan ekosistem gambut, dan mengembangkan kriteria dan klasifikasi tingkat kekritisan ekosistem gambut. Pengumpulan data dilaksanakan pada berbagai tipe penutupan hutan dan tingkat keterbukaan lahan gambut di Trumon dan Singkil, Provinsi Aceh. Analisis data meliputi analisis korelasi bivariat, analisis gerombol, dan analisis diskriminan. Karakteristik biofisik yang diukur adalah dinamika kedalaman muka air tanah, penurunan permukaan tanah, tingkat dekomposisi, unsur hara, kehilangan karbon, dan penutupan lahan. Hasil penelitian menunjukkan perubahan penutupan lahan dan pembangunan drainase mempengaruhi tingkat kekritisan ekosistem gambut. Perubahan tingkat dekomposisi gambut (nisbah C/N), perubahan kemasaman (pH) dan dinamika kedalaman muka air tanah merupakan penciri penting tingkat kekritisan ekosistem gambut. Ketiga faktor penciri ini diharapkan menjadi masukan dalam penyempurnaan kriteria tingkat kekritisan lahan pada Permenhut No. P.32/Menhut-II/2009 terutama pada ekosistem gambut.ABSTRACTPeat swamp forest is one specific and complex ecosystem. The limited understanding of the biophysical characteristics and critical properties are some root of problems peat ecosystem degradation in Indonesia. Generalizing in application of critical land criterions caused incorrect assessment, therefore the rehabilitation and management programs became ineffective. The objectives of the study was to determine the biophysical factors that influence the degree of criticality of peat ecosystem, and to develop criterion and classification of the criticality degree on peat ecosystem. Data collection was conducted on variety of forest cover types in Trumon and Singkil, Aceh Province. Data analysis included bivariate correlation analysis, analysis of clusters, and discriminant analysis. Biophysical characteristics were measured including the dynamics of the depth of the water table, rate of subsidence, level of decomposition, nutrient content, loss of carbon, and land/forest cover. Results showed land use change and drainage affects the critical level of peatland ecosystems. The change on level of peat decomposition (C/N ratio), soil acidity (pH) and groundwater dynamics were the identifier of critical peatland ecosystems. In addition to the criteria in Regulation No. P.32 / Menhut-II/2009, the identifier factors were expected to be considered in the refinement of the criteria of the critical level of peat ecosystem.
KEHILANGAN KARBON AKIBAT DRAINASE DAN DEGRADASI LAHAN GAMBUT TROPIKA DI TRUMON DAN SINGKIL ACEH (Carbon Loss from Drainaged and Degradation of Tropical Peatland in Trumon and Singkil, Aceh) Aswandi Aswandi; Ronggo Sadono; Haryono Supriyo; Hartono Hartono
Jurnal Manusia dan Lingkungan Vol 23, No 3 (2016): September
Publisher : Pusat Studi Lingkungan Hidup Universitas Gadjah Mada

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.22146/jml.18807

Abstract

ABSTRAKEkosistem hutan gambut tropika merupakan penyimpan karbon potensial, tetapi konversi lahan dan penebangan tidak lestari menyebabkan ekosistem ini juga menjadi sumber emisi karbon ke atmosfer. Pengaruh perubahan penutupan lahan dan pembangunan drainase terhadap dinamika muka air, penurunan tanah dan kehilangan karbon masih belum banyak diketahui pada tipologi gambut pesisir dengan bentang lahan yang sempit. Penelitian dilaksanakan pada berbagai tipe penutupan lahan gambut di Trumon dan Singkil, Provinsi Aceh mulai Mei 2013 hingga Oktober 2014. Penyimpanan dan kehilangan karbon dihitung berdasarkan bobot isi, kadar abu, karbon organik tanah, dan kedalaman tanah. Hasil penelitian menunjukkan perubahan penutupan lahan dan pembangunan drainase mempengaruhi tata air, penurunan tanah, dan kehilangan karbon sebesar 38,54 – 58,52%. Penurunan permukaan tanah tertinggi sebesar 5,6 cm/tahun terjadi pada lahan dengan bobot isi rendah dan intensitas drainase yang tinggi. Kehilangan karbon dari degradasi lahan gambut melepaskan sekitar1,352 ton CO2 eq/ha/tahun.  ABSTRACTTropical peat forest is one of significant atmospheric carbon sequester, but land conversion and illegal logging affects carbon stocks and transform these ecosystem into source of carbon emissions. The influence of land use change and drainage on water table fluctuation, soil subsidence and carbon loss are insufficiently known especially on typhology of narrow marine peatland. A study was conducted in Trumon and Singkil, Aceh Province from May 2012 until October 2014 in various peat land use types. Carbon stocks and carbon loss were calculated from data of bulk density, ash and carbon content, and peat depth. Results showed that land use types and distance from drainage influences the level of water table depth, subsidence rate, and carbon loss 38.54 – 58.52%. The highest subsidence rate occurred on peatlands which low bulk density and highly drainage intensity. Carbon loss from peat degradation released flux 1.352 ton CO2 eq/ha/year, highly correlated with measured rates of subsidence, depth of water table and bulk density.