不同生物质材料对蕉园土壤有机质组成的影响
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摘要
为探究不同生物质材料对蕉园土壤有机质及组成的影响,以木炭、椰壳炭、椰糠炭和与椰糠炭等碳量的椰糠为材料,分别以质量分数为2%和4%的用量加入土壤中,于室内常温培养并保持土壤含水量不变。在第15、30、60、90、120和180 d采集土壤,分析不同生物质材料对土壤有机质、胡敏酸、富里酸和土壤胡敏酸/富里酸的影响。结果表明:添加木炭、椰壳炭、椰糠炭和椰糠均能提高土壤有机质含量,并随添加量的增加而升高;添加木炭、椰壳炭、椰糠炭和椰糠均能加速土壤有机质的分解,添加椰壳炭对土壤有机质分解的影响相对较小。椰糠的添加主要是同时增加了土壤胡敏酸和富里酸碳含量,生物炭(木炭、椰壳炭和椰糠炭)的添加主要是影响了土壤胡敏酸与富里酸的相互转化。
In order to explore the effect of different biomass materials on the content and composition of organic matter in the soil of planting banana trees,in this study,charcoal,coconut shell charcoal,coconut bran charcoal and coconut bran with carbon content equal to coconut bran charcoal were used as the research materials,biomass materials were added to air-dried soil at rates of 2% and 4%(w/w)separately,then cultured them at room temperature and maintained soil moisture content. Soil organic matter content,humic acid carbon content and fulvic acid carbon content were tested after 15,30,60,90,120 and 180 days culture.The results showed that adding charcoal,coconut shell charcoal,coconut bran charcoal and coconut bran improved soil organic matter content and the effect increased with the increase of adding quantity.The decomposition of soil organic matter was accelerated by adding charcoal,coconut shell charcoal,coconut bran charcoal and coconut bran,but the effect of coconut charcoal was relatively small.Adding the coconut bran mainly increased the soil humic acid and fulvic acid carbon content at the same time,adding biochar(charcoal,coconut shell charcoal and coconut bran charcoal)mainly affected the conversion of soil humic acid and fulvic acid reciprocally.
In order to explore the effect of different biomass materials on the content and composition of organic matter in the soil of planting banana trees,in this study,charcoal,coconut shell charcoal,coconut bran charcoal and coconut bran with carbon content equal to coconut bran charcoal were used as the research materials,biomass materials were added to air-dried soil at rates of 2% and 4%(w/w)separately,then cultured them at room temperature and maintained soil moisture content. Soil organic matter content,humic acid carbon content and fulvic acid carbon content were tested after 15,30,60,90,120 and 180 days culture.The results showed that adding charcoal,coconut shell charcoal,coconut bran charcoal and coconut bran improved soil organic matter content and the effect increased with the increase of adding quantity.The decomposition of soil organic matter was accelerated by adding charcoal,coconut shell charcoal,coconut bran charcoal and coconut bran,but the effect of coconut charcoal was relatively small.Adding the coconut bran mainly increased the soil humic acid and fulvic acid carbon content at the same time,adding biochar(charcoal,coconut shell charcoal and coconut bran charcoal)mainly affected the conversion of soil humic acid and fulvic acid reciprocally.
引文
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[12]金素素.生物质炭施用对土壤CO2释放和碳截留影响的研究[D].西安:陕西科技大学,2013.
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[14]花莉,金素素,洛晶晶.生物质炭输入对土壤微域特征及土壤腐殖质的作用效应研究[J].生态环境学报,2012,21(11):1795-1799.
[15]葛立立,马义虎,卞金龙,等.玉米秸秆还田与实地氮肥管理对水稻产量与米质的影响[J].中国水稻科学,2013,27(2):153-160.
[16]Chen X,Xu Y J,Gao H J,et al.Biochemical stabilization of soil organic matter in straw-amended,anaerobic and aerobic soils[J].Science of the Total Environment,2018,625:1065-1073.
[17]周运来.秸秆还田方式对土壤有机碳固定及作物产量的影响[D].扬州:扬州大学,2017.
[18]赵世翔,于小玲,李忠徽,等.不同温度制备的生物质炭对土壤有机碳及其组分的影响:对土壤腐殖物质组成及性质的影响[J].环境科学,2017,38(2):769-782.
[19]Siewert C,Ku erík J,Tokarski D,et al.Linking soil organic matter thermal stability with contents of clay,bound water,organic carbon and nitrogen[J].Geoderma,2018,316:38-46.
[20]母媛,袁大刚,兰永生,等.植茶年限对土壤pH值、有机质与酚酸含量的影响[J].中国土壤与肥料,2016,(4):44-48.
[21]许毛毛.秸秆与秸秆炭对土壤碳库及养分的影响[D].哈尔滨:东北农业大学,2016.
[22]Kuzyakov Y.Priming effects:Interactions between living and dead organic matter[J].Soil Biology&Biochemistry,2010,42(9):1363-1371.
[23]Uchimiya M,Chang S C,Klasson K T.Screening biochars for heavy metal retention in soil:Role of oxygen functional groups[J].Journal of Hazardous Materials,2011,190:432-441.
[24]王鑫,王金成,刘建新.不同恢复阶段人工沙棘林土壤腐殖质组成及性质[J].水土保持通报,2014,34(5):49-54.
[25]董建伟.绿化混凝土上草坪植物所需营养元素及供给[J].吉林水利,2004,(2):1-5.
[26]赵世翔,于小玲,李忠徽,等.不同温度制备的生物质炭对土壤有机碳及其组分的影响:对土壤腐殖物质组成及性质的影响[J].环境科学,2017,38(2):769-782.
[27]黄惠群,蔡文昌,张健瑜,等.生物炭对紫色土中腐植酸淋溶的影响[J].中国土壤与肥料,2018,(4):48-54.
[28]Hung W N,Lin T F,Chiu C H,et al.On the use of a freezedried versus an air-dried soil humic acid as a surrogate of soil organic matter for contaminant sorption[J].Environmental Pollution,2012,160(1):125-129.
[29]宋杨.冻融作用下外源有机质对东北耕地土壤中重金属Pb和Cd赋存形态的影响[D].长春:吉林大学,2012.
[30]胡诚,陈云峰,乔艳,等.秸秆还田配施腐熟剂对低产黄泥田的改良作用[J].植物营养与肥料学报,2016,22(1):59-66.
[31]王丽莉.温度和水分对土壤腐殖质形成与转化的影响[D].长春:吉林农业大学,2003.
[32]孟凡荣.施用生物质炭对土壤腐殖质组成及胡敏酸和黑碳结构的影响[D].长春:吉林农业大学,2016.
[33]刘鑫,窦森,李长龙,等.开垦年限对稻田土壤腐殖质组成和胡敏酸结构特征的影响[J].土壤学报,2016,53(1):137-145.
[34]陈鲜妮,来航线,田霄鸿.接种微生物条件下牛粪+麦秸堆腐过程有机组分的动态变化[J].农业环境科学学报,2009,28(11):2417-2421.
[2]刘亚龙.水稻土微生物群落结构及功能随植稻年限的变化:滩涂围垦稻田时间序列的案例研究[D].南京:南京农业大学,2014.
[3]窦森.土壤有机质[M].北京:科学出版社,2010.
[4]Rodriguez-Murillo J C,Almendros G,Knicker H.Wetland soil organic matter composition in a Mediterranean semiarid wetland(Las Tablas de Daimiel,Central Spain):Insight into different carbon sequestration pathways[J].Organic Geochemistry,2011,42(7):762-773.
[5]Rodríguez F J,Schlenger P,García-Valverde M.Monitoring changes in the structure and properties of humic substances following ozonation using UV-Vis,FTIR and 1H NMR techniques[J].Science of the Total Environment,2016,541:623-637.
[6]Zhou Y,Selvam A,Wong J W C.Evaluation of humic substances during co-composting of food waste,sawdust and Chinese medicinal herbal residues[J].Bioresource Technology,2014,168:229-234.
[7]刘敏,杨永锋,陈红丽.不同有机物配施化肥对植烟土壤腐殖质碳的影响[J].河南农业科学,2017,46(2):38-42.
[8]徐跃,姚天全.气候因素对土壤有机质组成和性质的影响[J].山地研究,1994,12(3):163-168.
[9]比买热木·阿不都艾海提,艾克拜尔·伊拉洪,热依汗古丽·阿布力孜,等.新疆典型草原黑钙土腐殖质组分的垂直变化规律[J].新疆农业科学,2012,49(5):954-960.
[10]张靓,梁成华,杜立宇,等.长期定位施肥条件下蔬菜保护地土壤微团聚体组成及有机质状况分析[J].沈阳农业大学学报,2007,38(3):331-335.
[11]Ahmad M,Rajapaksha A U,Lim J E,et al.Biochar as a sorbent for contaminant management in soil and water:a review[J].Chemosphere,2014,99(3):19-33.
[12]金素素.生物质炭施用对土壤CO2释放和碳截留影响的研究[D].西安:陕西科技大学,2013.
[13]周桂玉,窦森,刘世杰.生物质炭结构性质及其对土壤有效养分和腐殖质组成的影响[J].农业环境科学学报,2011,30(10):2075-2080.
[14]花莉,金素素,洛晶晶.生物质炭输入对土壤微域特征及土壤腐殖质的作用效应研究[J].生态环境学报,2012,21(11):1795-1799.
[15]葛立立,马义虎,卞金龙,等.玉米秸秆还田与实地氮肥管理对水稻产量与米质的影响[J].中国水稻科学,2013,27(2):153-160.
[16]Chen X,Xu Y J,Gao H J,et al.Biochemical stabilization of soil organic matter in straw-amended,anaerobic and aerobic soils[J].Science of the Total Environment,2018,625:1065-1073.
[17]周运来.秸秆还田方式对土壤有机碳固定及作物产量的影响[D].扬州:扬州大学,2017.
[18]赵世翔,于小玲,李忠徽,等.不同温度制备的生物质炭对土壤有机碳及其组分的影响:对土壤腐殖物质组成及性质的影响[J].环境科学,2017,38(2):769-782.
[19]Siewert C,Ku erík J,Tokarski D,et al.Linking soil organic matter thermal stability with contents of clay,bound water,organic carbon and nitrogen[J].Geoderma,2018,316:38-46.
[20]母媛,袁大刚,兰永生,等.植茶年限对土壤pH值、有机质与酚酸含量的影响[J].中国土壤与肥料,2016,(4):44-48.
[21]许毛毛.秸秆与秸秆炭对土壤碳库及养分的影响[D].哈尔滨:东北农业大学,2016.
[22]Kuzyakov Y.Priming effects:Interactions between living and dead organic matter[J].Soil Biology&Biochemistry,2010,42(9):1363-1371.
[23]Uchimiya M,Chang S C,Klasson K T.Screening biochars for heavy metal retention in soil:Role of oxygen functional groups[J].Journal of Hazardous Materials,2011,190:432-441.
[24]王鑫,王金成,刘建新.不同恢复阶段人工沙棘林土壤腐殖质组成及性质[J].水土保持通报,2014,34(5):49-54.
[25]董建伟.绿化混凝土上草坪植物所需营养元素及供给[J].吉林水利,2004,(2):1-5.
[26]赵世翔,于小玲,李忠徽,等.不同温度制备的生物质炭对土壤有机碳及其组分的影响:对土壤腐殖物质组成及性质的影响[J].环境科学,2017,38(2):769-782.
[27]黄惠群,蔡文昌,张健瑜,等.生物炭对紫色土中腐植酸淋溶的影响[J].中国土壤与肥料,2018,(4):48-54.
[28]Hung W N,Lin T F,Chiu C H,et al.On the use of a freezedried versus an air-dried soil humic acid as a surrogate of soil organic matter for contaminant sorption[J].Environmental Pollution,2012,160(1):125-129.
[29]宋杨.冻融作用下外源有机质对东北耕地土壤中重金属Pb和Cd赋存形态的影响[D].长春:吉林大学,2012.
[30]胡诚,陈云峰,乔艳,等.秸秆还田配施腐熟剂对低产黄泥田的改良作用[J].植物营养与肥料学报,2016,22(1):59-66.
[31]王丽莉.温度和水分对土壤腐殖质形成与转化的影响[D].长春:吉林农业大学,2003.
[32]孟凡荣.施用生物质炭对土壤腐殖质组成及胡敏酸和黑碳结构的影响[D].长春:吉林农业大学,2016.
[33]刘鑫,窦森,李长龙,等.开垦年限对稻田土壤腐殖质组成和胡敏酸结构特征的影响[J].土壤学报,2016,53(1):137-145.
[34]陈鲜妮,来航线,田霄鸿.接种微生物条件下牛粪+麦秸堆腐过程有机组分的动态变化[J].农业环境科学学报,2009,28(11):2417-2421.
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