School of Life Science, Ludong University, Yantai 264025, China.
Institute of Geography & Planning, Ludong University, Yantai 264025, China.
Sci Total Environ. 2016 Nov 1;569-570:390-394. doi: 10.1016/j.scitotenv.2016.06.082. Epub 2016 Jun 25.
This study assessed the effects of temperature and moisture on carbon mineralization (Cmin) in a saline soil system with biochar amendment. The dynamics of Cmin were monitored in a biochar-amended saline soil for 220days by incubation experiments under different conditions of temperature (15°C, 25°C and 35°C) and moisture (30%, 70% and 105% of the water-holding capacity). Results showed that as the incubation temperature rose, cumulative Cmin consistently increased in soil added with 0-4% biochar. The two-compartment model could well describe the dynamics of Cmin. The temperature rise increased the concentration of labile C in soil, but reduced the turnover time of labile and recalcitrant C pools and the value of temperature coefficient Q10. The response of Cmin to moisture was varying in soil amended with different levels of biochar. In the control treatment (soil alone), cumulative Cmin increased only when soil moisture was >105%. In the biochar treatments, however, 70% of water-holding capacity was optimal for Cmin, except for 2%-biochar treatment at 35°C. The findings highlight the necessity to consider the combined effects of soil moisture, temperature and the amount of biochar added for assessing Cmin in biochar-amended saline soils.
本研究评估了温度和水分对添加生物炭的盐渍土壤系统中碳矿化(Cmin)的影响。通过在不同温度(15°C、25°C 和 35°C)和水分条件(持水能力的 30%、70%和 105%)下进行 220 天的培养实验,监测了添加生物炭的盐渍土壤中 Cmin 的动态。结果表明,随着培养温度的升高,添加 0-4%生物炭的土壤中累积 Cmin 持续增加。双区模型可以很好地描述 Cmin 的动态。温度升高增加了土壤中易分解碳的浓度,但降低了易分解和难分解碳库的周转时间和 Q10 值。水分对不同生物炭添加水平土壤中 Cmin 的响应不同。在对照处理(仅土壤)中,只有当土壤水分>105%时,累积 Cmin 才会增加。然而,在生物炭处理中,除了 35°C 时的 2%-生物炭处理外,70%的持水能力最有利于 Cmin。研究结果强调了在评估添加生物炭的盐渍土壤中的 Cmin 时,必须考虑土壤水分、温度和添加生物炭量的综合影响。