植物营养与肥料学报
植物營養與肥料學報
식물영양여비료학보
PLANT NUTRITION AND FERTILIZER SCIENCE
2009年
4期
831-836
,共6页
佟小刚%黄绍敏%徐明岗%卢昌艾%张文菊
佟小剛%黃紹敏%徐明崗%盧昌艾%張文菊
동소강%황소민%서명강%로창애%장문국
长期施肥%潮土%有机碳组分%分布
長期施肥%潮土%有機碳組分%分佈
장기시비%조토%유궤탄조분%분포
long-term fertilization%fluvo-aquic soil%organic carbon fractions%distribution
采用物理分组方法分析了长期不同施肥模式条件下潮土有机碳组分变化及其分布规律.结果表明,与不施肥(CK)比较,长期氮、磷、钾平衡施用(NPK)、秸秆还田(NPKS)和有机无机肥配施(NPKM和1.5NPKM)均显著提高了潮土粗自由颗粒有机碳(cfPOC)、微团聚体内物理保护颗粒有机碳(iPOC)及矿物结合有机碳(mSOC)的含量,其中以粗自由颗粒有机碳增幅最高,达114.5%~278.9%,对施肥最敏感,能较好地反映长期施肥下土壤有机碳库的变化.矿物结合有机碳是潮土固存有机碳的主要形式,它占总有机碳的67.0%~80.4%.除偏施化肥(N和NP)外,其他施肥模式增加的总有机碳的49.1%~58.1%进入矿物结合有机碳组分;26.2%~31.7%进入粗、细自由颗粒有机碳组分;15.7%~20.9%进入物理保护有机碳组分.偏施化肥(N和NP)有利于自由颗粒有机碳的增加.综上分析,长期有机无机肥配施或秸秆还田是提升潮土不同组分有机碳库较好的施肥模式.
採用物理分組方法分析瞭長期不同施肥模式條件下潮土有機碳組分變化及其分佈規律.結果錶明,與不施肥(CK)比較,長期氮、燐、鉀平衡施用(NPK)、秸稈還田(NPKS)和有機無機肥配施(NPKM和1.5NPKM)均顯著提高瞭潮土粗自由顆粒有機碳(cfPOC)、微糰聚體內物理保護顆粒有機碳(iPOC)及礦物結閤有機碳(mSOC)的含量,其中以粗自由顆粒有機碳增幅最高,達114.5%~278.9%,對施肥最敏感,能較好地反映長期施肥下土壤有機碳庫的變化.礦物結閤有機碳是潮土固存有機碳的主要形式,它佔總有機碳的67.0%~80.4%.除偏施化肥(N和NP)外,其他施肥模式增加的總有機碳的49.1%~58.1%進入礦物結閤有機碳組分;26.2%~31.7%進入粗、細自由顆粒有機碳組分;15.7%~20.9%進入物理保護有機碳組分.偏施化肥(N和NP)有利于自由顆粒有機碳的增加.綜上分析,長期有機無機肥配施或秸稈還田是提升潮土不同組分有機碳庫較好的施肥模式.
채용물리분조방법분석료장기불동시비모식조건하조토유궤탄조분변화급기분포규률.결과표명,여불시비(CK)비교,장기담、린、갑평형시용(NPK)、갈간환전(NPKS)화유궤무궤비배시(NPKM화1.5NPKM)균현저제고료조토조자유과립유궤탄(cfPOC)、미단취체내물리보호과립유궤탄(iPOC)급광물결합유궤탄(mSOC)적함량,기중이조자유과립유궤탄증폭최고,체114.5%~278.9%,대시비최민감,능교호지반영장기시비하토양유궤탄고적변화.광물결합유궤탄시조토고존유궤탄적주요형식,타점총유궤탄적67.0%~80.4%.제편시화비(N화NP)외,기타시비모식증가적총유궤탄적49.1%~58.1%진입광물결합유궤탄조분;26.2%~31.7%진입조、세자유과립유궤탄조분;15.7%~20.9%진입물리보호유궤탄조분.편시화비(N화NP)유리우자유과립유궤탄적증가.종상분석,장기유궤무궤비배시혹갈간환전시제승조토불동조분유궤탄고교호적시비모식.
The density fractionation scheme was used to study the changes of organic carbon fractions and their distribu-tion in fluvo-aquic soil under different long-term fertilizations. The results showed that compared to no fertilization (CK), contents of coarse free particulate organic carbon (cfPOC), physical protected intra-microaggregate particulate organic carbon (iPOC) and mineral-associated soil organic carbon(mSOC) were all increased significantly under the balanced chemical fertilization(NPK), straws plus with chemical fertilization (NPKS), and manure added with chemical fertiliza-tion (NPKM and 1.5NPKM). The cfPOC fraction with the highest magnitude of increased by 114.5%-278.9% indi-cates it was more sensitive to the fertilizations than other organic carbon fractions. The mSOC, accounting for 67.0% to 80.4% of total organic carbon (TOC), was main form for organic carbon sequestration in fluvo-aquic soil. Application of unbalanced chemical fertilization (N and NP) was apt to increase free POC content, and for other fertilizations, about 49.1% -58.1% of TOC was transferred to mSOC, 26.2% -31.7% to free POC and 15.7% -20.9% to iPOC. It could be concluded that long-term manure application with chemical fertilizers or straw incorporation to soil was more ben-efit to organic carbon pools upgrade in fluvo-aquic soil.