A global study on the natural dynamics and land-use impacts on tropical peat soil properties and greenhouse gas effluxes

2021 ◽  
Author(s):  
Sigit D Sasmito ◽  
Pierre Taillardat ◽  
Letisha Fong ◽  
Jonathan Ren ◽  
Hanna Sundahl ◽  
...  
2019 ◽  
Vol 17 (3) ◽  
pp. 1703-1712 ◽  
Author(s):  
C. Agus ◽  
Z. R. Ilfana ◽  
F. F. Azmi ◽  
D. Rachmanadi ◽  
Widiyatno ◽  
...  

2021 ◽  
Vol 9 ◽  
Author(s):  
Lisbet Norberg ◽  
Maria Hellman ◽  
Kerstin Berglund ◽  
Sara Hallin ◽  
Örjan Berglund

Greenhouse gas emissions from drained agricultural peatlands contribute significantly to global warming. In a laboratory study using intact cores of peat soil from eight different sites in Sweden, factors controlling the emission of the greenhouse gases nitrous oxide (N2O) and methane (CH4) were examined. Soil properties, and the abundance of the total microbial community (16S rRNA gene abundance), and genes encoding for functions controlling N2O emissions (bacterial and archaeal amoA, nirS, nirK, nosZI, and nosZII) were analyzed and compared against measured greenhouse gas emissions. Emissions were measured at different drainage levels, i.e., higher soil water suction values, since drainage is an important factor controlling greenhouse gas emissions from peat soils. The results showed that N2O and CH4 emissions were generally low, except for N2O emissions at near water-saturated conditions, for which three soils displayed high values and large variations in fluxes. Relationships between N2O emissions and soil properties were mainly linked to soil pH, with higher emissions at lower pH. However, specific assemblages of nitrogen cycling guilds that included nosZII, typically present in non-denitrifying N2O reducers, were detected in soils with low N2O emissions. Overall, these results indicate that both pH and biotic controls determine net N2O fluxes.


2001 ◽  
Vol 16 (2) ◽  
pp. 79-86 ◽  
Author(s):  
Abdul Hadi ◽  
Muhammad Haridi ◽  
Kazuyuki Inubushi ◽  
Erry Purnomo ◽  
Fadly Razie ◽  
...  

2005 ◽  
Vol 71 (1) ◽  
pp. 81-91 ◽  
Author(s):  
Yuichiro Furukawa ◽  
Kazuyuki Inubushi ◽  
Mochamad Ali ◽  
A. M. Itang ◽  
Haruo Tsuruta

2020 ◽  
Vol 52 (1) ◽  
pp. 61
Author(s):  
Rossie Wiedya Nusantara ◽  
Sudarmadji Sudarmadji ◽  
Tjut S. Djohan ◽  
Eko Haryono

The conversion of tropical peat forest to other land uses can reduce organic carbon (C) and stable C isotope (δ13C) of peat soil. This research aimed at analyzing the soil organic-C and δ13C of peatland with respect to maturity (fibric, hemic and sapric) in five types of peatland use, which included primary peat forest, secondary peat forest, shrubs, oil palm plantations, and cornfield in West Kalimantan. Analysis of peat soil samples includes organic C with Loss in ignition method and δ13C  using an isotope ratio mass spectrometry(IRMS) method. Organic-C at fibric was higher than hemic and sapric, respectively (57.2%, 57.0%, 56.4%), meanwhile, organic-C was the highest on primary peat forest, followed by on secondary peat forest, oil palm plantation, cornfield, and shrubs, respectively 57.1%, 57.0%, 56.4%, 56.0%. The cause of increasing and decreasing organic C and δ13C due to land-use change due to changes in vegetation, burning during tillage, and age of organic matter of peat soil. This condition causes the opening of natural peat ecosystems and changes in anaerobic to aerobic conditions. 


2019 ◽  
Vol 5 (1) ◽  
pp. 1708683
Author(s):  
Gebrejewergs Aredehey ◽  
Gebremedhn Berhe Zenebe ◽  
Aklil Gebremedhn ◽  
Manuel Tejada Moral

2010 ◽  
Vol 7 (11) ◽  
pp. 3403-3419 ◽  
Author(s):  
G. Z. Anshari ◽  
M. Afifudin ◽  
M. Nuriman ◽  
E. Gusmayanti ◽  
L. Arianie ◽  
...  

Abstract. Degradation of tropical peats is a global concern due to large Carbon emission and loss of biodiversity. The degradation of tropical peats usually starts when the government drains and clears peat forests into open peats used for food crops, oil palm and industrial timber plantations. Major properties of tropical peat forests are high in Water Contents (WC), Loss on Ignition (LOI) and Total Organic Carbon (TOC), and low in peat pH, Dry Bulk Density (DBD), and Total Nitrogen (TN). In this study, we investigated impacts of drainage and land use change on these properties. We collected peat samples from peat forests, logged over peat forest, industrial timber plantation, community agriculture, and oil palms. We used independent t-tests and oneway ANOVA to analyze mean differences of the research variables. We found that peat pH, DBD, and TN tend to increase. A significant decrease of C/N ratio in oil palm and agriculture sites importantly denotes a high rate of peat decompositions. Water contents, LOI, and TOC are relatively constants. We suggest that changes in pH, DBD, TN and atomic C/N ratio are important indicators for assessing tropical peat degradation. We infer that land use change from tropical peat forests into cleared and drained peats used for intensive timber harvesting, oil palms and industrial timber plantations in Indonesia has greatly degraded major ecological function of tropical peats as Carbon storage.


Soil Research ◽  
2012 ◽  
Vol 50 (5) ◽  
pp. 390
Author(s):  
Wentai Zhang ◽  
David C. Weindorf ◽  
Yuanda Zhu ◽  
Beatrix J. Haggard ◽  
Noura Bakr

Human-induced soil change is attracting increasing attention, yet how to quantitatively measure anthropogenic impact on changes in soil properties remains unclear. Eight selected soil properties—bulk density (BD), sand, silt, and clay content, pH, soil organic matter (SOM), total carbon (TC), and total nitrogen (TN)—at four soil depths (0–10, 10–20, 20–30, and 30–40 cm) were measured across three soil series (Gallion, Latanier and Sharkey) in south-central Louisiana, USA, to quantify changes in soil properties as a function of three contrasting land use types, i.e. forest, cropland, and Wetlands Reserve Program. Partial eta-squared values (η2) derived from two-way analysis of variance were used to quantitatively compare natural factors (soil series) and anthropogenic impact (land use) on these soil properties. Results showed that properties such as BD, pH, SOM, TC, and TN could be easily changed by anthropogenic disturbance, especially at 0–10 cm, while soil texture was mainly a natural factor. The anthropogenic factor accounted for 55.2%, 39.5%, 33.2%, and 36.0% of changes in the soil properties at 0–10, 10–20, 20–30, and 30–40 cm depth, respectively. These findings highlight the anthropogenic impact on selected soil properties.


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