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GREENHOUSE GAS (GHG) EMISSIONS IN RELATION TO WATER TABLE AND SOIL AMELIORATION FROM TROPICAL PEAT SOILS

机译:温室气体(GHG)与热带泥炭土壤的水位和土壤改善有关的排放

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Tropical peatlands could be a source of greenhouse gases (GHG) as they contain large amounts of soil carbon (C). In order to be suitable for cultivation, peatlands must be drained, limed and fertilised due to the excess water, acidic soil properties and low soil fertility. On the other hand, drainage and soil amelioration may influence GHG emissions. This study was conducted with the aim to understand the effect of water table depth and soil amelioration on GHG emissions on tropical peat soils. Peat soil columns from Central Kalimantan, Indonesia were used to estimate GHG emissions under different water tables and soil amelioration treatments. Twenty seven peat columns were arranged using a randomized block design with two factors; water table position at 15 cm, 35 cm and 55 cm from the soil surface, and secondly 3 different ameliorants: without ameliorant/control, biochar (2.5 tonnes ha~(-1)) + compost (2.5 t ha"1); steel slag (2.5 t ha"1) + compost (2.5 t ha"1). Each of the treatments was replicated three times. Carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) emissions from the peat soil columns were measured at weekly intervals for 92 days and analysed using gas chromatography in the Indonesian Agricultural Environment Research Institute (IAERI). Results showed that soil ameliorations influenced CO2 and N2Q emissions from the peat soil. As application of soil ameliorants tended to stimulate GHG emissions, amelioration of peat soils to enhance soil fertility should be more wisely considered due to the effect on GHG emissions. Estimated GHG emissions from the treatments were between 0.12-0.32 kg CO2-C column~(-1) 92 days~(-1). Water tables affected the C-stock and net CO2-C exchange in peat soil columns.
机译:热带泥炭地可能是温室气体的来源(GHG),因为它们含有大量的土壤碳(C)。为了适合培养,由于水,酸性土壤性质过多,土壤肥力低,必须排出,泥炭地净化和施肥。另一方面,排水和土壤改善可能影响温室气体排放。本研究旨在了解水位深度和土壤改善对热带泥炭土壤的温室气体排放的影响。来自印度尼西亚中部的卡利莫坦坦中部的泥炭土柱用于估计不同水表和土壤改善处理下的温室气体排放。使用具有两个因素的随机块设计来安排二十七个泥炭柱;距离土壤表面15厘米,35厘米,55厘米的水位位置,其次3种不同的改进剂:没有修复/控制,生物炭(2.5吨HA〜(-1))+堆肥(2.5 T HA“1);钢炉渣(2.5 t ha“1)+堆肥(2.5 t ha”1)。每种处理被复制三次。二氧化碳(CO2),甲烷(CH4)和氧化氮(N 2 O)来自泥炭土壤柱的排放量按照每周间隔测量92天,并在印度尼西亚农业环境研究所(IAERI)中使用气相色谱分析。结果表明,土壤改造影响了泥炭土壤的二氧化碳和N2Q排放。作为土壤修复师的应用趋于刺激温室气体排放,改善由于对温室气体排放的影响,应更明智地考虑泥炭土壤以提高土壤肥力。治疗的估计温室气体排放量为0.12-0.32kg CO2-C柱〜(-1)92天〜(-1)。水桌子影响了泥炭土壤中的C股和净二氧化碳兑换MNS。

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