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首页> 外文期刊>Archives of Agronomy and Soil Science >Response of soils properties and archaea community to saline-sodic soils under long-term rice-based cropping system
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Response of soils properties and archaea community to saline-sodic soils under long-term rice-based cropping system

机译:长期水稻种植制度下土壤性质和古细菌群落对盐碱土壤的响应

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Understanding the soil microbiology and physico-chemistry may contribute to efficient land utilization. A 10-year field experiment was conducted in Songnen Plain, China. High-throughput sequencing and quantitative PCR of 16S rRNA and methyl coenzyme M reductase A (mcrA) genes were performed to investigate the dynamic changes in archaeal community following long-term rice planting. Ten-year rice planting significantly decreased soil salinity and alkalinity, including pH (7.6), electrical conductivity (23.9), sodium absorption ratio (33.1), and exchangeable sodium percentage (33.5) and significantly increased soil organic carbon (70.5) and mineral nutrient concentrations. Rice planting increased alpha-diversity, and reshaped the archaea community structure of saline-alkali soil. The archaea community compositions during the 10-year period were divided into three stages: 1) shift in abundance from ammonia-oxidizing archaea to methanogenic archaea, 2) methanogenic archaea (e.g. genera Methanosarcina, Methanosaeta, Methanobacterium, Methanocella, Methanomassiliicoccus) established superiority, and 3) methanogenic archaea genes copy numbers increased and the community became stable. Redundancy analysis showed that the decrease in pH caused by long-term flooding was the main factor responsible for the changes in archaea community structure. The results highlighted that the rice planting could be a beneficial approach for maintaining ecological stability and reclaiming severe saline-alkali soil.
机译:了解土壤微生物学和物理化学可能有助于有效利用土地。在中国松嫩平原进行了为期10年的野外试验。采用高通量测序和定量PCR技术对16S rRNA和甲基辅酶M还原酶A(mcrA)基因进行高通量测序和定量PCR,研究长期水稻种植后古菌群落的动态变化。10年水稻种植显著降低了土壤盐碱度,包括pH值(7.6%)、电导率(23.9%)、钠吸收率(33.1%)和可交换钠含量(33.5%),土壤有机碳(70.5%)和矿质养分浓度显著增加。水稻种植增加了盐碱土的α多样性,重塑了古菌群落结构。10年间古细菌群落组成分为3个阶段:1)丰度由氨氧化古菌向产甲烷古菌转变;2)产甲烷古菌(如Methanosarcina属、Methanosaeta属、甲酸杆菌属、甲烷菌属、甲烷菌属)确立了优势;3)产甲烷古菌基因拷贝数增加,群落趋于稳定。冗余分析表明,长期淹水导致的pH值降低是导致古细菌群落结构变化的主要因素。结果表明,水稻种植对维护生态稳定、恢复严重盐碱土具有重要意义。

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