Effect of land-use changes on nitrous oxide (N2O) emission from tropical peatlands

Abdul Hadi , K Inubushi , E Purnomo , F Razie , K Yamakawa , H Tsuruta
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引用次数: 69

Abstract

Tropical peatlands could be a potential source of nitrous oxide (N2O) which has a significant impact on global warming. To reduce N2O emission and develop best management practices for peatlands, the formation and emission rates of N2O as affected by land-use management (i.e., changing peatland into agricultural land) and the factors affecting the process must be understood. Therefore, one field and three laboratory incubation experiments were carried out during 1998–99 using peatland soils from 12 sites in South Kalimantan (Indonesia) and one site in Sarawak (Malaysia) to quantify the N2O emission and the factors affecting it. The results from the field experiment showed that land-use managements, changing water table and locations had a significant impact on N2O emission. Changing peatland into cultivated lands (cultivated upland and paddy field) enhanced the N2O emission. For example, cultivated upland Cassava crop resulted in the highest amounts of N2O emission (1.04 mg N m−2 h−1) compared to other treatments. The N2O emission during 1998 was higher than those during 1999 because of the changing water table and dry season in 1998. The laboratory experiments showed that the N2O emission was also strongly influenced by land-use management, soil moisture contents, addition of ammonium fertilizer or rice straw and soil depths. For example, the flooded conditions stimulated the N2O emission compared to that at 60% moisture contents. Similarly, the addition of ammonium fertilizer suppressed the N2O emission compared to control treatments because of the high ammonium contents that inhibit nitrification. Nevertheless, incorporation of rice straw to soil samples from 20 to 40 cm soil depth stimulated N2O emission.

土地利用变化对热带泥炭地氧化亚氮排放的影响
热带泥炭地可能是对全球变暖有重大影响的一氧化二氮(N2O)的潜在来源。为了减少一氧化二氮的排放并制定泥炭地的最佳管理措施,必须了解受土地利用管理(即将泥炭地转变为农业用地)影响的一氧化二氮的形成和排放率以及影响这一过程的因素。因此,在1998 - 1999年期间,利用南加里曼丹(印度尼西亚)12个地点和沙捞越(马来西亚)一个地点的泥炭地土壤进行了一次实地和三次实验室孵化试验,以量化N2O排放及其影响因素。田间试验结果表明,土地利用管理、地下水位和位置变化对N2O排放有显著影响。泥炭地变为耕地(耕地和水田)增加了N2O的排放。例如,与其他处理相比,旱地木薯作物的N2O排放量最高(1.04 mg N m−2 h−1)。由于1998年地下水位变化和旱季的影响,1998年N2O排放量高于1999年。室内试验表明,N2O排放还受土地利用管理、土壤含水量、施用铵肥或稻草以及土壤深度的强烈影响。例如,与60%含水率相比,淹水条件刺激了N2O的排放。同样,与对照处理相比,铵肥的添加抑制了N2O的排放,因为高铵含量抑制了硝化作用。然而,在土壤深度20 ~ 40 cm的土壤样品中掺入稻草会促进N2O的排放。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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