摘要
为了解地膜覆盖对菜地剖面温室气体的影响,本研究利用扩散箱法测定了2014—2015年西南地区辣椒-萝卜轮作菜地10、20和30 cm土壤剖面的CH4、CO_(2)和N2O的浓度.结果表明,整个观测季覆膜(F)和不覆膜(NF)处理土壤剖面的CH4浓度均随土壤深度增加而降低.与NF相比,覆膜极显著提高了辣椒季30 cm土层的CH4浓度(p<0.01),但极显著降低了萝卜季20 cm土层的CH4浓度(p<0.01),且对观测季其他土层的CH4浓度无显著影响(p>0.05);与CH4相反,整个观测季覆膜和不覆膜处理土壤剖面的CO_(2)浓度均随土壤深度增加而增加.与NF相比,覆膜显著提高了辣椒季30 cm土层和萝卜季各土层的CO_(2)浓度(p<0.05);与CO_(2)相似,整个观测季节覆膜和不覆膜处理土壤剖面的N2O浓度均随土壤深度增加而增加.与NF相比,覆膜对辣椒季各土层的N2O浓度影响不显著(p<0.05),却显著增加了萝卜季各土层的N2O浓度(p<0.05).总之,在辣椒季,地膜覆盖有利于深层土壤(30 cm)CH4和CO_(2)的积累,而对N2O的影响却不显著.在萝卜季,地膜覆盖不利于中层土壤(20 cm)CH4的积累,但有利于各土层CO_(2)和N2O的积累.Pearson相关性分析结果表明,在辣椒季,各处理10 cm土层的CH4浓度与土壤充水孔隙度(WFPS)呈显著正相关(p<0.05),各处理10 cm土层的CO_(2)浓度与各环境因子相关性均不显著(p>0.05).与CO_(2)类似,覆膜处理10 cm土层的N2O浓度与各环境因子相关性不显著(p>0.05),但不覆膜处理10 cm土层的N2O浓度与WFPS呈显著正相关(p<0.05).在萝卜季,各处理10 cm土层的CH4浓度与各环境因子相关性不显著(p>0.05),各处理10 cm土层的CO_(2)和N2O浓度与地下10 cm温度和土壤氮素呈显著正相关(p<0.05).WFPS是影响10 cm土层CH4浓度的主要因素,土壤温度和土壤氮素是影响10 cm土层CO_(2)浓度的主要因素,WFPS、土壤温度和土壤氮素是影响10 cm土层N2O浓度的主要因素.
In order to understand the effect of plastic film mulching on greenhouse gases in vegetable soil profiles, the concentration of CH4, CO_(2) and N2O in soils with depth of 10, 20 and 30 cm profiles of pepper-radish rotation vegetable fields in southwestern China were measured by diffusion box method during 2014—2015. The results showed that the CH4 concentration of the treated soil profiles with film mulching(F) and no film mulching(NF) decreased with increasing soil depth during the whole observation period. Compared with NF, the film mulching significantly increased CH4 concentration in 30 cm soil layer in pepper growing season(p<0.01), but significantly decreased CH4 concentration in 20 cm soil layer in radish growing season(p<0.01), and had no significant effect on CH4 concentration in other soil layer during observation season(p>0.05);Contrary to CH4, the CO_(2) concentrations of the F and NF-treated soil profiles increased with increasing soil depth during the whole observation period. Compared with NF, the film mulching significantly increased the CO_(2) concentration in the soil layer of 30 cm in pepper growing season and the all soil layers of radish growing season(p<0.05);Similar to CO_(2), the N2O concentrations of the F and NF-treated soil profiles increased with increasing soil depth during the entire observation season. Compared with NF, the influence of film mulching on N2O concentration in soil layers was not significant(p<0.05) in pepper growing season. However, it significantly increased the N2O concentration of all soil layers in radish growing season(p<0.05). In short, in the pepper growing season, mulching film is beneficial to the accumulation of CH4 and CO_(2) in the deep soil(30 cm), but the effect on N2O is not significant. In the radish season, plastic film mulching is not conducive to the accumulation of CH4 in the middle soil(20 cm), but it is conducive to the accumulation of CO_(2) and N2O in each soil layer. Pearson correlation analysis results showed that, in the pepper growing season, the CH4 concentrations of the F and NF-treated 10 cm soil profile were significantly positively correlated with the soil water filled pore space(WFPS)(p<0.05), while the CO_(2) concentrations of the F and NF-treated 10 cm soil profile were not significantly correlated with various environmental factors(p>0.05). Similar to CO_(2), the N2O concentration of the F-treated 10 cm soil profile was not significantly correlated with various environmental factors(p>0.05), but the N2O concentration of the NF-treated in 10 cm soil profile was significantly positively correlated with WFPS(p<0.05). In the radish growing season, the CH4 concentrations of the F and NF-treated 10 cm soil profile were not significantly correlated with various environmental factors(p>0.05). The CO_(2) and N2O concentrations of the F and NF-treated 10 cm soil profile were significantly positively correlated with the temperature of 10 cm underground and soil nitrogen(p<0.05). The effect of plastic film mulching on the greenhouse gases concentration of soil profiles is not consistent in different planting seasons WFPS is the main factor affecting the concentration of CH4 in the 10 cm profile. Soil temperature and soil nitrogen are the main factors affecting the concentration of CO_(2) in the 10 cm profile. WFPS, soil temperature and soil nitrogen are the main factors affecting the concentration of N2O in the 10 cm profile.
作者
陈俊江
江长胜
熊维霞
赵仲婧
曾唯
郝庆菊
CHEN Junjiang;JIANG Changsheng;XIONG Weixia;ZHAO Zhongjing;ZENG Wei;HAO Qingju(State Cultivation Base of Eco-agriculture for Southwest Mountainous Land,College of Resources and Environment,Southwest University,Chongqing 400716;Key Laboratory of Eco-environments in Three Gorges Reservoir Region of Ministry of Education,Chongqing 400715)
出处
《环境科学学报》
CAS
CSCD
北大核心
2021年第3期1134-1141,共8页
Acta Scientiae Circumstantiae
基金
重庆市基础研究与前沿探索专项(No.cstc2018jcyjAX0476,cstc2019jcyj-msxmX0425)
国家自然科学基金(No.41275160,41977186)。
关键词
地膜覆盖
菜地
土壤剖面
温室气体
plastic film mulching
vegetable field
soil profiles
greenhouse gases
