globalchange  > 气候变化与战略
CSCD记录号: CSCD:5480462
论文题名:
三江平原沼泽湿地垦殖对土壤微生物学性质影响研究
其他题名: Effects of Marshland Reclamation on Soil Microbial Properties in the Sanjiang Plain, Northeast China
作者: 宫超; 宋长春; 谭稳稳; 张加双
刊名: 生态环境学报
ISSN: 1674-5906
出版年: 2015
卷: 24, 期:6, 页码:156-159
语种: 中文
中文关键词: 沼泽湿地 ; 土壤有机碳 ; 微生物量碳 ; 土壤呼吸商 ; 三江平原 ; 垦殖
英文关键词: marshland ; SOC ; microbial biomass carbon ; soil metabolic quotient ; Sanjiang Plain ; reclamation
WOS学科分类: ENVIRONMENTAL SCIENCES
WOS研究方向: Environmental Sciences & Ecology
中文摘要: 沼泽湿地垦殖对全球碳循环有重要影响,可以对全球气候系统产生反馈调节作用。土壤微生物学指标是反映不同土地利用方式最敏感的指示因子,可以在早期反映土壤有机碳的变化情况。以我国三江平原典型沼泽湿地、湿地垦殖为水田(15 a)和旱田(25 a)3种土地利用方式为研究对象,开展了沼泽湿地垦殖对土壤微生物学性质变化影响研究。结果表明,沼泽湿地垦殖为水田和旱田后土壤有机碳、全氮含量显著降低(P=0.001),其中有机碳平均降低了31.50%、51.38%,全氮降低了49.81%、63.88%,旱田减少量显著高于水田,垦殖后全氮损失量高于有机碳引起土壤质量的下降。湿地开垦后土壤微生物量碳和土壤基础呼吸显著降低(P<0.001),土壤有机质和养分可利用性下降,微生物活性降低,但开垦后二者在0~10和10~20 cm土层间的差异变弱;微生物熵总体表现为降低趋势,旱田和沼泽湿地0~10 cm土层差异不显著(P=0.728),10~20 cm土层差异显著(P=0.005),反映出农田土壤活性有机碳分配比例的降低;湿地垦殖后,水田土壤呼吸商(qCO_2)升高,而旱田qCO_2值显著降低(P=0.003),说明微生物在不同土地利用方式下对底物基质碳源利用策略发生改变;经回归分析发现,qCO_2和土壤有机碳、全氮含量呈显著正相关,表明微生物对基质碳利用率随土壤质量的改善而降低。
英文摘要: Reclamation of marshland to farmland has great effects on global carbon cycling and inducing feedbacks to global climate change. Soil microbial properties are the most sensitive and indicative factors of land use changes that can reflect the dynamics of soil organic carbon (SOC) in the early stage. This study took the typical marsh wetland, wetland reclamation to paddy field (15 a) and soybean field (25 a) as the objectives to research the effects of reclamation on the soil microbial properties in the Sanjiang Plain, Northeast China. The results showed that the contents of SOC and total nitrogen (TN) were significantly decreased after marshland reclamation (P<0.001). The average SOC content was reduced by 31.50%, 51.38% and 49.81%, 63.88% of TN, respectively. The reduction of soybean field was higher than that of paddy field and the high TN reduction relative to SOC induced the decrease of soil quality. The soil microbial biomass carbon (MBC) and basal soil respiration (BR) were also significantly decreased (P<0.001), the availability of SOC and nutrients decreased and caused the decline of the microbial activity. Meanwhile, the differences of MBC and BR between 0~10 cm and 10~20 cm soil layers weakened and the heterogeneity decreased after reclamation. The microbial quotient showed a decreasing trend and the difference in 0~10 cm soil layer of soybean field and wetland was not significant (P=0.728), while that of 10~20 cm was significantly different (P=0.005), reflecting the decrease of soil labile organic allocation after reclamation. The soil metabolic quotient (qCO_2) of paddy field increased and that of soybean field significantly decreased (P=0.003) indicating the varied microbial carbon use efficiency of different land use types. The qCO_2 had significantly positive correlations with SOC and TN by regression analysis, suggesting that the substrate use efficiency of soil microbes decreased with the improvement of soil nutrients condition. This study manifests that the soil biogeochemical cycling will be greatly influenced by the changed microbial properties.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/149735
Appears in Collections:气候变化与战略

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作者单位: 中国科学院东北地理与农业生态研究所, 中国科学院湿地生态与环境重点实验室, 长春, 吉林 130102, 中国

Recommended Citation:
宫超,宋长春,谭稳稳,等. 三江平原沼泽湿地垦殖对土壤微生物学性质影响研究[J]. 生态环境学报,2015-01-01,24(6):156-159
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