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[水溶性有机物和凋落物残体对亚热带森林土壤氮转化的影响。]

[Effects of water-soluble organic matter and residue of litter on nitrogen transformation in subtropical forest soil.].

作者信息

Ma Fen, Pei Guang Ting, Ma Hong Liang, Gao Ren, Yin Yun Feng, Yang Liu Ming

机构信息

Cultivation Base of State Key Laboratory of Humid Subtropical Mountain Ecology, Fuzhou 350007, China.

College of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2016 Sep;27(9):2761-2770. doi: 10.13287/j.1001-9332.201609.006.

Abstract

An incubation experiment was carried out with the addition of litter filtrate, litter residue and alanine at 25 ℃ for 36 days under 60% and 90%WHC (water holding capacity) conditions. The results showed that alanine was rapidly mineralized in soil, and soil NH-N content significantly increased by 5.4%-44.7% and 16.1%-41.3%, respectively under 60% and 90%WHC conditions compared with the control. The soil net nitrogen mineralization and ammonification rates in the two treatments were also higher than those in the control at the early stage of incubation. However, the soil NH-N content was reduced by the addition of filtrate and residue, and the reduction degree of residue was greater. During the incubation, soil NO-N content showed a linear increasing trend with the incubation time, and it was significantly higher under the 60%WHC condition than that under 90%WHC condition at the end of incubation. The mineralization of soil organic matter was limited by higher soil moisture. Therefore, the soil soluble organic carbon (SOC) content under 90%WHC condition was obviously lower than that under 60%WHC, but nitrous oxide (NO) emission was 1.5-63.0 times higher than that under 60%WHC. Furthermore, NO emission was induced significantly by the addition of litter residue under 60%WHC condition. These results indicated that there were different effects of soluble matter and litter residue on soil nitrogen transformation, and these differences would change dynamically in the decomposition process.

摘要

在25℃下,分别在60%和90%的田间持水量(WHC)条件下,添加凋落物滤液、凋落物残渣和丙氨酸进行了36天的培养实验。结果表明,丙氨酸在土壤中迅速矿化,与对照相比,在60%和90%WHC条件下,土壤铵态氮(NH₄⁺-N)含量分别显著增加了5.4%-44.7%和16.1%-41.3%。在培养初期,两种处理的土壤净氮矿化率和氨化率也高于对照。然而,添加滤液和残渣会降低土壤NH₄⁺-N含量,且残渣的降低程度更大。在培养期间,土壤硝态氮(NO₃⁻-N)含量随培养时间呈线性增加趋势,培养结束时,60%WHC条件下的含量显著高于90%WHC条件下的含量。较高的土壤湿度限制了土壤有机质的矿化。因此,90%WHC条件下的土壤可溶性有机碳(SOC)含量明显低于60%WHC条件下的,但氧化亚氮(N₂O)排放量比60%WHC条件下高1.5-63.0倍。此外,在60%WHC条件下,添加凋落物残渣显著诱导了N₂O排放。这些结果表明,可溶性物质和凋落物残渣对土壤氮转化有不同影响,且这些差异在分解过程中会动态变化。

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