摘要
为研究UV-A辐射增强对土壤-冬小麦系统微量气体释放的影响规律,通过室外盆栽试验,人工模拟UV-A辐射增强,UV-A辐射强度处理分别比自然光(CK)增加10%(T1)和20%(T2)。采用静态箱-气相色谱法测定了不同UV-A辐射强度下裸土、土壤-冬小麦系统的呼吸速率和N2O排放通量。结果表明:T1和T2处理下裸土呼吸速率分别比CK高83%(P=0.022)和263%(P=0.038),T2处理比T1高99%(P=0.073);T1和T2处理使裸土N2O排放通量比CK分别增加了64%(P=0.019)和186%(P=0.059),但T2与T1处理间的N2O排放通量差异不显著(P=0.123)。UV-A辐射增强没有显著影响土壤-冬小麦系统的呼吸速率大小;T2处理下土壤-冬小麦系统的N2O排放通量显著高于CK(P=0.012)和T1(P=0.010),分别比CK和T1高33%和40%,但T1和CK的N2O排放通量无显著差异(P=0.352)。UV-A辐射增强没有影响冬小麦生物量(P>0.05),但T2处理下土壤-冬小麦系统的土壤微生物碳和亚硝酸氧化菌的数量明显高于对照。
Extensive work has been done to understand the effect of enhanced UV-B (280-320 nm) radiation because of the depletion of the stratospheric ozone layer on plants, however, the available information related to the effect of UV-A (320-400 nm) on plants or ecosystem is limited. It merits further studies due to the facts that UV-A constitutes a major portion of the solar radiation and passes through the stratospheric ozone layer almost unattenuated. To investigate the impact of enhanced UV-A radiation on trace gases emission from bare soil and soil-winter wheat system, outdoor pot experiments with simulating 0%(CK), 10% (T1) and 20% (T2) supplement of UV-A were conducted, and static dark chamber-gas chromatograph method were used to measure respiration rate and N2O emission fluxes. Results indicated that enhanced UV-A radiation increased respiration rate and N2O emission fluxes in bare soil, soil respiration rates of T1 and T2 were 1.83 and 3.63 times larger than those of CK (P=0.022, 0.038, respectively), and soil respiration rates of T2 were 1.99 times larger than those of T1 (P= 0.073). N2O emission fluxes in bare soil of T1 and T2 were 1.64 and 2.86 times larger than that of CK (P=0.019, 0.059, respectively), while there no significant difference between T2 fluxes and T1 fluxes (P=0.123). Enhanced UV-A radiation had no significant impact on respiration rate of soil-winter Wheat system, but 20% supplemental UV-A radiation increased significantly N2O emission fluxes from soil-winter wheat system,N2O emission fluxes of T2 were 1.33 and 1.40 times larger than those of CK (P=0.012) and T1 (P=0.010), while T1 and CK had no significant difference in N2O emission fluxes (P=0.352). In addition, enhanced UV-A radiation had no significant impact on biomass of winterwheat (P〉0.05), but soil microbial biomass C and nitrite-oxidation bacteria quantity of T2 were obviously higher than those of CK.
出处
《农业环境科学学报》
CAS
CSCD
北大核心
2008年第5期1860-1865,共6页
Journal of Agro-Environment Science
基金
国家自然科学基金项目(40605029)
中国科学院大气物理研究所大气边界层物理和大气化学国家重点实验室开放课题(LAPC-KF-2004-03)