植物营养与肥料学报
植物營養與肥料學報
식물영양여비료학보
PLANT NUTRITION AND FERTILIZER SCIENCE
2014年
3期
525-533
,共9页
宋震震%李絮花%李娟%林治安%赵秉强
宋震震%李絮花%李娟%林治安%趙秉彊
송진진%리서화%리연%림치안%조병강
长期施肥%有机肥%化肥%土壤活性有机氮组分%土壤酶活性
長期施肥%有機肥%化肥%土壤活性有機氮組分%土壤酶活性
장기시비%유궤비%화비%토양활성유궤담조분%토양매활성
long-term fertilization%organic fertilizer%mineral fertilizer%soil labile nitrogen fraction%soil enzyme activity
本文以中国农业科学院山东禹城长期定位施肥试验为平台,研究了长期施用有机肥和化肥26年后对土壤活性氮库不同组分[颗粒有机氮(POM-N)、可溶性有机氮(DON)、微生物量氮(SMBN)及轻组有机氮(LFOM-N)]及土壤酶活性的影响。结果表明,与不施肥相比,长期施肥显著提高了土壤全氮、颗粒有机氮、可溶性有机氮、微生物量氮以及轻组有机氮的含量,长期施有机肥效果好于化肥,施用高量有机肥效果好于施用常量有机肥。常量施用量下,50%有机肥和50%化肥配施处理其土壤全氮和活性有机氮库各组分含量与高量化肥处理的相当。长期施化肥处理土壤全氮及活性有机氮库各组分含量随施肥量的增加而显著增高。 POM-N对土壤全氮的贡献率最高,且明显受施肥方式的影响,LFOM-N对土壤全氮的贡献率不随施肥方式的改变而变化。长期施肥处理土壤脲酶、碱性磷酸酶和蔗糖酶活性显著增加,它们之间及与土壤全氮、速效磷及有机碳含量间呈现显著或极显著相关性,脲酶活性与土壤各活性氮组分间也存在显著或极显著相关性;但长期施肥后土壤过氧化氢酶的活性低于不施肥处理。
本文以中國農業科學院山東禹城長期定位施肥試驗為平檯,研究瞭長期施用有機肥和化肥26年後對土壤活性氮庫不同組分[顆粒有機氮(POM-N)、可溶性有機氮(DON)、微生物量氮(SMBN)及輕組有機氮(LFOM-N)]及土壤酶活性的影響。結果錶明,與不施肥相比,長期施肥顯著提高瞭土壤全氮、顆粒有機氮、可溶性有機氮、微生物量氮以及輕組有機氮的含量,長期施有機肥效果好于化肥,施用高量有機肥效果好于施用常量有機肥。常量施用量下,50%有機肥和50%化肥配施處理其土壤全氮和活性有機氮庫各組分含量與高量化肥處理的相噹。長期施化肥處理土壤全氮及活性有機氮庫各組分含量隨施肥量的增加而顯著增高。 POM-N對土壤全氮的貢獻率最高,且明顯受施肥方式的影響,LFOM-N對土壤全氮的貢獻率不隨施肥方式的改變而變化。長期施肥處理土壤脲酶、堿性燐痠酶和蔗糖酶活性顯著增加,它們之間及與土壤全氮、速效燐及有機碳含量間呈現顯著或極顯著相關性,脲酶活性與土壤各活性氮組分間也存在顯著或極顯著相關性;但長期施肥後土壤過氧化氫酶的活性低于不施肥處理。
본문이중국농업과학원산동우성장기정위시비시험위평태,연구료장기시용유궤비화화비26년후대토양활성담고불동조분[과립유궤담(POM-N)、가용성유궤담(DON)、미생물량담(SMBN)급경조유궤담(LFOM-N)]급토양매활성적영향。결과표명,여불시비상비,장기시비현저제고료토양전담、과립유궤담、가용성유궤담、미생물량담이급경조유궤담적함량,장기시유궤비효과호우화비,시용고량유궤비효과호우시용상량유궤비。상량시용량하,50%유궤비화50%화비배시처리기토양전담화활성유궤담고각조분함량여고양화비처리적상당。장기시화비처리토양전담급활성유궤담고각조분함량수시비량적증가이현저증고。 POM-N대토양전담적공헌솔최고,차명현수시비방식적영향,LFOM-N대토양전담적공헌솔불수시비방식적개변이변화。장기시비처리토양뇨매、감성린산매화자당매활성현저증가,타문지간급여토양전담、속효린급유궤탄함량간정현현저혹겁현저상관성,뇨매활성여토양각활성담조분간야존재현저혹겁현저상관성;단장기시비후토양과양화경매적활성저우불시비처리。
In this paper, the effects of long-term application of organic fertilizer and chemical fertilizer on soil labile nitrogen fractions and some kinds of soil enzyme activities ( urease, catalase, alkaline phosphatase and sucrase ) were studied based on a 26-year long-term field experiment in Chinese Academy of Agricultural Sciences Research Station in Yucheng City, Shandong province, China.The results show that, compared with CK, long term fertilization significantly increases soil total nitrogen , particle organic nitrogen ( POM-N ) , dissolved organic nitrogen ( DON ) , microbial biomass nitrogen ( MBN ) and light fraction organic nitrogen ( LFON ) contents . Treatments of applying organic fertilizers alone could improve soil total nitrogen and labile nitrogen fractions contents more effectively than the treatments of applying mineral fertilizers alone .The highest soil total nitrogen and labile nitrogen fractions contents appear in treatment of double organic fertilizer input , then is the treatment of common organic fertilizer input .The similar soil total nitrogen and labile nitrogen fraction contents are in treatment of applying 50%organic fertilizer and 50% mineral fertilizer and the treatment of applied double amount of mineral fertilizers.The soil total nitrogen and labile nitrogen fraction contents are improved with the increased input levels of mineral fertilizers .POM-N is the main contributor of the soil total nitrogen , affected by fertilizer types and input levels.There is no difference in the contribution of LFOM-N to the soil total nitrogen among all the treatments , suggesting that fertilizer application types and input levels couldn ’ t affect the contribution of LFOM-N to the soil total nitrogen.The activities of soil urease , alkaline phosphatase and sucrase are increased significantly by the application of fertilizers .The three enzyme activities are correlated significantly with each other , and also correlated with soil total nitrogen , available phosphorus and organic carbon , and closer correlation exists between the urease activity and soil labile nitrogen fractions contents .But the activity of soil catalase is decreased after long-term application of fertilizers.