Taiki Mori, S. Ishizuka, R. Konda, A. Wicaksono, J. Heriyanto, A. Hardjono, S. Ohta
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We prepared P-added soils (Ca(H2PO4)2, 20 μg P g soil ) and non-added control to test the effects of P addition on N2O emissions. Contrary to our hypothesis, P addition did not reduce N2O emissions, although soil microbial N immobilization was stimulated by P addition in soils with low C addition. Stimulated total N cycling by P addition probably offset the decrease in soil inorganic N. Meanwhile P addition reduced soil microbial biomass N (MBN) content in H60, where N2O emissions increased significantly by P addition. It was possible that the microbial growth reached its peak and started dying more quickly in P-added soils in H60 due to the favorable condition for microbes (higher C and water content). 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引用次数: 10
摘要
在相对好氧条件下,研究了添加磷(P)对锰相思人工林土壤氧化亚氮(N2O)排放的影响,同时添加碳(C)和氮(N)。我们假设P的添加通过刺激微生物N固定和随后产生N2O的无机N资源减少来减少N2O的排放。我们准备了以下四组实验;高碳(葡萄糖2000 μ C g土壤)和充水孔隙(WFPS) 40% (H40),低碳(葡萄糖100 μ C g土壤)和充水孔隙(WFPS) 40% (L40),高碳和充水孔隙(WFPS) 60% (H60),低碳和充水孔隙(WFPS) 60% (L60)。所有土壤均添加氮(NH4NO3, 20 μg N g土壤)。制备了加磷土壤(Ca(H2PO4)2, 20 μ P g土壤)和未加磷对照,考察了加磷对N2O排放的影响。与我们的假设相反,添加P并没有减少N2O的排放,尽管在低碳添加的土壤中,添加P可以促进土壤微生物的N固定。施磷促进了土壤总氮循环,可能抵消了土壤无机氮的减少,同时施磷降低了H60土壤微生物生物量N (MBN)含量,其中N2O排放量显著增加。在H60加磷土壤中,微生物生长达到峰值,开始死亡的速度更快,可能是由于微生物的有利条件(较高的C和含水量)。因此,我们得出结论:(1)添加磷并不一定促进土壤微生物氮的固定;(2)即使添加磷促进土壤微生物氮的固定,N2O的排放也可能不会减少。
Effects of phosphorus addition on N2O emissions from an Acacia mangium soil in relatively aerobic condition
Effects of phosphorus (P) addition on nitrous oxide (N2O) emissions from an Acacia mangium plantation soil was examined in relatively aerobic condition with carbon (C) and nitrogen (N) addition. We hypothesized that P addition reduced N2O emissions through stimulated microbial N immobilization and subsequent decrease in inorganic N resources for producing N2O. We prepared the following four experimental sets; high C (glucose 2000 μg C g soil ) and water-filled pore space (WFPS) 40 % (H40), low C (glucose 100 μg C g soil) and WFPS 40 % (L40), high C and WFPS 60 % (H60), and low C and WFPS 60 % (L60). Nitrogen (NH4NO3, 20 μg N g soil ) was also added to all soils. We prepared P-added soils (Ca(H2PO4)2, 20 μg P g soil ) and non-added control to test the effects of P addition on N2O emissions. Contrary to our hypothesis, P addition did not reduce N2O emissions, although soil microbial N immobilization was stimulated by P addition in soils with low C addition. Stimulated total N cycling by P addition probably offset the decrease in soil inorganic N. Meanwhile P addition reduced soil microbial biomass N (MBN) content in H60, where N2O emissions increased significantly by P addition. It was possible that the microbial growth reached its peak and started dying more quickly in P-added soils in H60 due to the favorable condition for microbes (higher C and water content). Thus we concluded that (i) P addition did not necessarily stimulate soil microbial N immobilization, and (ii) N2O emissions might not decrease even if P addition stimulated soil microbial N immobilization.