Interaction of Peat Soil and Sulphidic Material Substratum: Role of Peat Layer and Groundwater Level Fluctuations on Phosphorus Concentration

Phosphorus (P) often becomes limiting factor for plants growth. Phosphorus geochemistry in peatland soil is associated with the presence of peat layer and groundwater level fluctuations. The research was conducted to study the role of peat layer and groundwater level fluctuations on P concentration...

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Main Author: Benito Heru Purwanto
Format: Article
Language:English
Published: University of Lampung 2014-09-01
Series:Journal of Tropical Soils
Subjects:
Online Access:http://journal.unila.ac.id/index.php/tropicalsoil/article/view/918
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author Benito Heru Purwanto
author_facet Benito Heru Purwanto
author_sort Benito Heru Purwanto
collection DOAJ
description Phosphorus (P) often becomes limiting factor for plants growth. Phosphorus geochemistry in peatland soil is associated with the presence of peat layer and groundwater level fluctuations. The research was conducted to study the role of peat layer and groundwater level fluctuations on P concentration in peatland. The research was conducted on deep, moderate and shallow peat with sulphidic material as substratum, peaty acid sulphate soil, and potential acid sulphate soil. While P concentration was observed in wet season, in transition from wet to dry season, and in dry season. Soil samples were collected by using peat borer according to interlayer and soil horizon. The results showed that peat layer might act as the main source of P in peatland with sulphidic material substratum. The upper peat layer on sulphidic material caused by groundwater level fluctuations had no directly effect on P concentration in the peat layers. Increased of P concentration in the lowest sulphidic layer might relate to redox reaction of iron in the sulphidic layer and precipitation process. Phosphorus concentration in peatland with sulphidic material as substratum was not influenced by peat thickness. However, depletion or disappearance of peat layer decreased P concentration in soil solution. Disappearance of peat layer means loss of a natural source of P for peatland with sulphidic material as substratum, therefore peat layer must be kept in order to maintain of peatlands.
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spelling doaj.art-5136f074773b4a459de0863bcd2399062022-12-22T00:38:14ZengUniversity of LampungJournal of Tropical Soils0852-257X2086-66822014-09-0119317117910.5400/jts.2014.19.3.171Interaction of Peat Soil and Sulphidic Material Substratum: Role of Peat Layer and Groundwater Level Fluctuations on Phosphorus ConcentrationBenito Heru Purwanto0Soil Science Division, Faculty of Agriculture, Gadjah Mada University, YogyakartaPhosphorus (P) often becomes limiting factor for plants growth. Phosphorus geochemistry in peatland soil is associated with the presence of peat layer and groundwater level fluctuations. The research was conducted to study the role of peat layer and groundwater level fluctuations on P concentration in peatland. The research was conducted on deep, moderate and shallow peat with sulphidic material as substratum, peaty acid sulphate soil, and potential acid sulphate soil. While P concentration was observed in wet season, in transition from wet to dry season, and in dry season. Soil samples were collected by using peat borer according to interlayer and soil horizon. The results showed that peat layer might act as the main source of P in peatland with sulphidic material substratum. The upper peat layer on sulphidic material caused by groundwater level fluctuations had no directly effect on P concentration in the peat layers. Increased of P concentration in the lowest sulphidic layer might relate to redox reaction of iron in the sulphidic layer and precipitation process. Phosphorus concentration in peatland with sulphidic material as substratum was not influenced by peat thickness. However, depletion or disappearance of peat layer decreased P concentration in soil solution. Disappearance of peat layer means loss of a natural source of P for peatland with sulphidic material as substratum, therefore peat layer must be kept in order to maintain of peatlands.http://journal.unila.ac.id/index.php/tropicalsoil/article/view/918Groundwater levelpeat soilphosphorussoil chemical propertiessulphidic material
spellingShingle Benito Heru Purwanto
Interaction of Peat Soil and Sulphidic Material Substratum: Role of Peat Layer and Groundwater Level Fluctuations on Phosphorus Concentration
Journal of Tropical Soils
Groundwater level
peat soil
phosphorus
soil chemical properties
sulphidic material
title Interaction of Peat Soil and Sulphidic Material Substratum: Role of Peat Layer and Groundwater Level Fluctuations on Phosphorus Concentration
title_full Interaction of Peat Soil and Sulphidic Material Substratum: Role of Peat Layer and Groundwater Level Fluctuations on Phosphorus Concentration
title_fullStr Interaction of Peat Soil and Sulphidic Material Substratum: Role of Peat Layer and Groundwater Level Fluctuations on Phosphorus Concentration
title_full_unstemmed Interaction of Peat Soil and Sulphidic Material Substratum: Role of Peat Layer and Groundwater Level Fluctuations on Phosphorus Concentration
title_short Interaction of Peat Soil and Sulphidic Material Substratum: Role of Peat Layer and Groundwater Level Fluctuations on Phosphorus Concentration
title_sort interaction of peat soil and sulphidic material substratum role of peat layer and groundwater level fluctuations on phosphorus concentration
topic Groundwater level
peat soil
phosphorus
soil chemical properties
sulphidic material
url http://journal.unila.ac.id/index.php/tropicalsoil/article/view/918
work_keys_str_mv AT benitoherupurwanto interactionofpeatsoilandsulphidicmaterialsubstratumroleofpeatlayerandgroundwaterlevelfluctuationsonphosphorusconcentration