首页> 外文会议>International Peat Congress >EFFECT OF FOREST TYPE ON DECOMPOSITION RATE AND GREENHOUSE GAS FLUXES OF TROPICAL PEAT SOIL AFTER CONVERSION INTO AN OIL PALM PLANTATION
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EFFECT OF FOREST TYPE ON DECOMPOSITION RATE AND GREENHOUSE GAS FLUXES OF TROPICAL PEAT SOIL AFTER CONVERSION INTO AN OIL PALM PLANTATION

机译:森林型对油棕种植后热带泥炭土壤分解率和温室气体助气的影响

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The effect of forest type on the decomposability and greenhouse gas fluxes of tropical peat soils after conversion to an oil palm plantation was evaluated through a field incubation experiment of peat soils from three representative types of primary forest in Sarawak, Malaysia, namely Mixed Peat Swamp (MPS), Alan Baru (ABt), and Alan Bunga (ABg). Carbon dioxide (CO2) and methane (CH4) fluxes were measured on a monthly basis for 36 months. The CO2 and CH4 fluxes ranged from 78-625 mg C m~(-2) h~(-1) and -67-653 p.g C ~(-2) h~(-1), respectively. Both of CO2 and CH4 fluxes were larger in the order ABg > ABt > MPS, which corresponded to the relative abundance of O-alkyl C derived mainly from polysaccharides in soil organic matter (SOM). Rate of decomposition of peat was almost constant during the 3-year period, and annual decomposition rate was estimated to be 0.033 y~(-1) for MPS, 0.048 y~(-1) for ABt. and 0.066 y~(-1) for ABg.
机译:通过来自马来西亚三种代表性的原发性森林的泥炭土壤的泥炭土壤的现场孵化试验评估了森林类型对热带泥炭土壤的分解性和温室气体势态的影响。混合泥炭沼泽( MPS),Alan Baru(ABT)和Alan Bunga(ABG)。二氧化碳(CO 2)和甲烷(CH4)助熔剂按月测量36个月。 CO 2和CH 4通量范围为78-625mg C m〜(-2)H〜(-1)和-67-653 p.g c〜(-2)h〜(-1)。在ABG> ABT> MPS的顺序中,两种CO 2和CH 4助熔剂均较大,这对应于主要来自土壤有机物质中的多糖的O-烷基C的相对丰度(SOM)。泥炭的分解率几乎恒定在3年期间,每年分解率为MPS为0.033 y〜(-1),为ABT为0.048 y〜(-1)。为ABG为0.066 y〜(-1)。

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