scholarly journals Drainage of organic soils and GHG emissions: Validation with country data

2020 ◽  
Author(s):  
Giulia Conchedda ◽  
Francesco N. Tubiello

Abstract. Drainage of large areas with organic soils was conducted over the past century to free land for agriculture. A significant acceleration of such trends was observed in recent decades in South-East Asia, largely driven by drainage of tropical peatlands, an important category of organic soils, for cultivation of oil palm. This work presents methods and main results of a new methodology developed for FAOSTAT, whereby the overlay of dynamic maps of land cover and the use of information on histosols allows the production of a global annual dataset of drained area and emissions over a time series, covering the period 1990–2019. This is an improvement over the existing FAO approach, which had produced only a static map of drained organic soils for the year 2000. Results indicate that drained area and emissions increased by 13 percent globally since 1990, reaching in 2019 24 million ha of drained organic soils, with world total emissions of 830 million tonnes of carbon dioxide (CO2) equivalent. Of these totals, the largest contribution was from the drainage of tropical peatlands in South-East Asia, generating nearly half of global emissions. Results were validated against national data reported by countries to the UN Climate Convention and to well established literature. Overall, the validation yielded a good agreement with these sources. FAOSTAT estimates explained about 60 percent of the variability in official country reported data. The predicted emissions were virtually identical – with over 90 percent of explained variability – to official data from Indonesia, currently the top emitting country by drained organic soils. Also, calculated emissions factors for oil palm plantations in Indonesia and Malaysia were in the same range and very close to emissions factors derived from detailed field measurements. This validation suggests that the FAO estimates may be a useful and sound reference in support of countries reporting needs. Data are made available as open access via the Zenodo portal (Tubiello and Conchedda, 2020) with DOI https://doi.org/10.5281/zenodo.3942370.

2020 ◽  
Vol 12 (4) ◽  
pp. 3113-3137
Author(s):  
Giulia Conchedda ◽  
Francesco N. Tubiello

Abstract. Drainage of large areas with organic soils was conducted over the past century to free up land for agriculture. A significant acceleration of such trends was observed in recent decades in Southeast Asia, largely driven by drainage of tropical peatlands, an important category of organic soils, for cultivation of oil palm. This work presents the methods and main results of a new methodology developed for FAOSTAT, whereby the overlay of dynamic maps of land cover and the use of information about histosols allows the production of a global annual dataset of drained area and emissions over a time series, covering the period 1990–2019. This is an improvement over the existing FAO approach, which had produced only a static map of drained organic soils for the year 2000. Results indicate that drained area and emissions increased by 13 % globally since 1990, reaching 24 million hectares in 2019 of drained organic soils, with world total emissions of 830 Mt of carbon dioxide (CO2) equivalent. Of these totals, the largest contribution was from the drainage of tropical peatlands in Southeast Asia, generating nearly half of global emissions. Results were validated against national data reported by countries to the UN Climate Convention and against the well-established literature. Overall, the validation yielded a good agreement with these sources. FAOSTAT estimates explained about 60 % of the variability in official country-reported data. The predicted emissions were virtually identical – with over 90 % of explained variability – to official data from Indonesia, currently the top emitting country by drained organic soils. Also, calculated emissions factors for oil palm plantations in Indonesia and Malaysia were in the same range and very close to emissions factors derived from detailed field measurements. This validation suggests that the FAO estimates may be a useful and sound reference in support of countries reporting needs. Data are made available through open access via the Zenodo portal (Tubiello and Conchedda, 2020) with the following DOI: https://doi.org/10.5281/zenodo.3942370.


2021 ◽  
Author(s):  
Nick Pasiecznik

Abstract E. guineensis, the oil palm or African oil palm, is native to equatorial Africa, although the only other species in the genus (E. oleifera) is indigenous to South and Central America. E. guineensis, however, is the major economic species: fruits of E. oleifera have a much lower oil content and are used only locally (Westphal and Jansen, 1989). However, E. guineensis was introduced into South America during the time of the slave trade, and naturalized groves are reported in coastal areas of Brazil near Bélem. In the mid-1800s it was introduced to South-East Asia via the Botanic Gardens in Bogor, Indonesia. The first oil-palm estates in Sumatra (since 1911) and Malaysia (since 1917) used plant material from second- and third-generation descendants of the original Bogor palms, from which one of the breeding populations, the Deli Dura, is derived (Westphal and Jansen, 1989). After soyabean, E. guineensis is the second most important crop worldwide for the supply of edible vegetable oil. Palm oil kernel, for example, is a major agricultural export from Malaysia, and South-East Asia is the main area of production.E. guineensis yields two types of oil: palm oil from the fleshy mesocarp, and palm-kernel oil from the kernel, in a volume ratio 10:1. Most palm oil is used in food preparation (margarines, and industrial frying oils used to prepare snack foods, etc.). Palm-kernel oil is similar in composition and properties to coconut oil, and is used in confectionery, where its higher melting point is particularly useful. It is also used in the manufacture of lubricants, plastics, cosmetics and soaps. The oil palm is a monoecious, erect, single-stemmed tree usually 20-30 m high. The root system is shallow and adventitious, forming a dense mat in the top 35 cm of the soil. The main stem is cylindrical, up to 75 cm diameter. E. guineensis palm fronds are not as suitable for thatching as other palm species, as the leaflets attach to the rachis at two angles. The oil palm is indigenous to the lowland humid tropics, and thrives on a good moisture supply and relatively open conditions. It can tolerate fluctuating water-tables with periods of standing water, although continuously flooded conditions are unsuitable. Sites often selected as suitable for oil palm are swamps, riverbanks, or sites considered too moist for tropical rain forest trees. Rainfall is often the major factor limiting production in plantations: highest yields occur where rainfall is evenly distributed throughout the year, with an optimum of 150 mm per month (Westphal and Jansen, 1989). Oil palms can grow on a variety of soil types, from sandy soils to lateritic red and yellow podzols, young volcanic soils, alluvial clays and peat soils; water-holding capacity appears to be the most important soil criterion. It is a demanding crop in terms of soil nutrients. The oil palm also has potential for incorporation into agroforestry practices. Traditional oil palm management in some areas of West Africa often incorporated both pure oil palm groves (perhaps selectively retained), scattered oil palms within temporary fields, and unexploited oil palms in mixed forest (Gupta, 1993). Harvesting of fruits usually starts about 2½ years after field planting; bunches ripen throughout the year and so harvesting usually takes place at intervals of 2 to 3 weeks in any particular area. Because oil palm is so responsive to environmental conditions, yields may vary greatly. However, over the lifetime of a palm tree, yields generally rise to a maximum in the first 6-8 years (after field planting), and will subsequently decline slowly. In Malaysia and Sumatra, well-managed plantations yield between 24 and 32 tonnes/hectare of fruit bunches; the oil yield from this will be between 4.8 and 7 tonnes/hectare. Oil palm plantations are often regarded as a better use of the land than annual food crops in humid tropical areas where soils are prone to leaching: the plantations provide continuous ground cover, and the palm canopy helps protect against soil erosion. Oil palm stems are increasingly used as a raw material for paper and composite board production. This area has big prospects in wood-based industries. It is recommended that more research is undertaken into the properties and utilization. Propagation techniques, the management of pests and diseases, and genetic resources are other areas in which studies could usefully be undertaken.


Author(s):  
R. R. M. Paterson ◽  
M. Holderness ◽  
J. Kelley ◽  
R. N. G. Miller ◽  
E. O'Grady

2019 ◽  
Vol 16 (23) ◽  
pp. 4687-4703 ◽  
Author(s):  
Jyrki Jauhiainen ◽  
Jukka Alm ◽  
Brynhildur Bjarnadottir ◽  
Ingeborg Callesen ◽  
Jesper R. Christiansen ◽  
...  

Abstract. Drained organic forest soils in boreal and temperate climate zones are believed to be significant sources of the greenhouse gases (GHGs) carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O), but the annual fluxes are still highly uncertain. Drained organic soils exemplify systems where many studies are still carried out with relatively small resources, several methodologies and manually operated systems, which further involve different options for the detailed design of the measurement and data analysis protocols for deriving the annual flux. It would be beneficial to set certain guidelines for how to measure and report the data, so that data from individual studies could also be used in synthesis work based on data collation and modelling. Such synthesis work is necessary for deciphering general patterns and trends related to, e.g., site types, climate, and management, and the development of corresponding emission factors, i.e. estimates of the net annual soil GHG emission and removal, which can be used in GHG inventories. Development of specific emission factors also sets prerequisites for the background or environmental data to be reported in individual studies. We argue that wide applicability greatly increases the value of individual studies. An overall objective of this paper is to support future monitoring campaigns in obtaining high-value data. We analysed peer-reviewed publications presenting CO2, CH4 and N2O flux data for drained organic forest soils in boreal and temperate climate zones, focusing on data that have been used, or have the potential to be used, for estimating net annual soil GHG emissions and removals. We evaluated the methods used in data collection and identified major gaps in background or environmental data. Based on these, we formulated recommendations for future research.


2011 ◽  
Vol 366 (1582) ◽  
pp. 3277-3291 ◽  
Author(s):  
William A. Foster ◽  
Jake L. Snaddon ◽  
Edgar C. Turner ◽  
Tom M. Fayle ◽  
Timothy D. Cockerill ◽  
...  

The conversion of natural forest to oil palm plantation is a major current threat to the conservation of biodiversity in South East Asia. Most animal taxa decrease in both species richness and abundance on conversion of forest to oil palm, and there is usually a severe loss of forest species. The extent of loss varies significantly across both different taxa and different microhabitats within the oil palm habitat. The principal driver of this loss in diversity is probably the biological and physical simplification of the habitat, but there is little direct evidence for this. The conservation of forest species requires the preservation of large reserves of intact forest, but we must not lose sight of the importance of conserving biodiversity and ecosystem processes within the oil palm habitat itself. We urgently need to carry out research that will establish whether maintaining diversity supports economically and ecologically important processes. There is some evidence that both landscape and local complexity can have positive impacts on biodiversity in the oil palm habitat. By intelligent manipulation of habitat complexity, it could be possible to enhance not only the number of species that can live in oil palm plantations but also their contribution to the healthy functioning of this exceptionally important and widespread landscape.


Mycologist ◽  
1998 ◽  
Vol 12 (1) ◽  
pp. 10-14 ◽  
Author(s):  
Roland Treu
Keyword(s):  
Oil Palm ◽  

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