The relationship between surface topography and peat thickness on Tebing Tinggi Island, Indonesia

Peat and its substratum have different geology and parent materials. Studies on peat formation and spatial patterns of peat deposits have been widely reported, but little is known about patterns of peat thickness across tropical peat landscapes. We studied the relationship between surface relief and...

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Main Authors: B. Nasrul, A. Maas, S.N.H. Utami, M. Nurudin
Format: Article
Language:English
Published: International Mire Conservation Group and International Peatland Society 2020-06-01
Series:Mires and Peat
Subjects:
Online Access:http://mires-and-peat.net/media/map26/map_26_18.pdf
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author B. Nasrul
A. Maas
S.N.H. Utami
M. Nurudin
author_facet B. Nasrul
A. Maas
S.N.H. Utami
M. Nurudin
author_sort B. Nasrul
collection DOAJ
description Peat and its substratum have different geology and parent materials. Studies on peat formation and spatial patterns of peat deposits have been widely reported, but little is known about patterns of peat thickness across tropical peat landscapes. We studied the relationship between surface relief and peat thickness on Tebing Tinggi Island (Indonesia) by considering peat surface altitude, peat thickness and substratum altitude. The research location is unique, being a small (~ 70 × 30 km) predominantly peat-covered island separated by a strait from the mainland of Sumatra and its more extensive peat deposits. Geomorphological features on the island were identified using a digital terrain model (DTM) developed from LiDAR data, together with observations on peat cores. The results indicate that the topography of the peat landscape does not reflect peat thickness. Thick peat can be found at the edge of a peat dome if it overlies a basin or valley in the substratum, while thinner peat can be found at the centre if it overlies a mound in the substratum. It is also important to note that the shapes of the peat surface and the substratum surface are not the same; a flat peatland surface may have an undulating substratum and vice versa.
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spelling doaj.art-68a08c2b5a8d43e79ab032700875f3212023-09-02T22:48:01ZengInternational Mire Conservation Group and International Peatland SocietyMires and Peat1819-754X2020-06-01261812110.19189/MaP.2019.OMB.StA.1811The relationship between surface topography and peat thickness on Tebing Tinggi Island, IndonesiaB. Nasrul0A. Maas1S.N.H. Utami2M. Nurudin3Study Program of Soil Science, Faculty of Agriculture, Universitas Riau, Tampan, Pekanbaru, and Department of Soil Science, Faculty of Agriculture, Universitas Gadjah Mada, Bulaksumur, Yogyakarta, IndonesiaDepartment of Soil Science, Faculty of Agriculture, Universitas Gadjah Mada, Bulaksumur, Yogyakarta, IndonesiaDepartment of Soil Science, Faculty of Agriculture, Universitas Gadjah Mada, Bulaksumur, Yogyakarta, IndonesiaDepartment of Soil Science, Faculty of Agriculture, Universitas Gadjah Mada, Bulaksumur, Yogyakarta, IndonesiaPeat and its substratum have different geology and parent materials. Studies on peat formation and spatial patterns of peat deposits have been widely reported, but little is known about patterns of peat thickness across tropical peat landscapes. We studied the relationship between surface relief and peat thickness on Tebing Tinggi Island (Indonesia) by considering peat surface altitude, peat thickness and substratum altitude. The research location is unique, being a small (~ 70 × 30 km) predominantly peat-covered island separated by a strait from the mainland of Sumatra and its more extensive peat deposits. Geomorphological features on the island were identified using a digital terrain model (DTM) developed from LiDAR data, together with observations on peat cores. The results indicate that the topography of the peat landscape does not reflect peat thickness. Thick peat can be found at the edge of a peat dome if it overlies a basin or valley in the substratum, while thinner peat can be found at the centre if it overlies a mound in the substratum. It is also important to note that the shapes of the peat surface and the substratum surface are not the same; a flat peatland surface may have an undulating substratum and vice versa.http://mires-and-peat.net/media/map26/map_26_18.pdflidar dtmmacrotopepeat domepeat surface altitudesubstratumsumatra
spellingShingle B. Nasrul
A. Maas
S.N.H. Utami
M. Nurudin
The relationship between surface topography and peat thickness on Tebing Tinggi Island, Indonesia
Mires and Peat
lidar dtm
macrotope
peat dome
peat surface altitude
substratum
sumatra
title The relationship between surface topography and peat thickness on Tebing Tinggi Island, Indonesia
title_full The relationship between surface topography and peat thickness on Tebing Tinggi Island, Indonesia
title_fullStr The relationship between surface topography and peat thickness on Tebing Tinggi Island, Indonesia
title_full_unstemmed The relationship between surface topography and peat thickness on Tebing Tinggi Island, Indonesia
title_short The relationship between surface topography and peat thickness on Tebing Tinggi Island, Indonesia
title_sort relationship between surface topography and peat thickness on tebing tinggi island indonesia
topic lidar dtm
macrotope
peat dome
peat surface altitude
substratum
sumatra
url http://mires-and-peat.net/media/map26/map_26_18.pdf
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