绿肥作物还田后腐解规律及对土壤肥力与玉米产量的影响
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
苜蓿、草木樨是东北地区主要的绿肥兼牧草作物。本文研究了绿肥作物苜蓿、草木樨还田翻压后的腐解规律以及翻压做绿肥对土壤肥力和玉米产量的影响,为在东北粮食主产区发展绿肥作物提供技术和理论支持。
     研究采用田间试验、室内实验分析结合的方法,于2008-2010年在黑龙江省富裕县沈阳军区富裕农副业进行。
     苜蓿、草木樨茎叶埋入土壤后其干物质的腐解及氮、磷、钾的矿化规律具有相同的趋势,腐解速率与气温的高低成正比,在每年的7月-8月之间是腐解及矿化最快的时期;两种绿肥钾的矿化都是在第一年就矿化了96%以上。试验结果表明:苜蓿和草木樨生物量两年的分解率分别为87.54%、90.18%,苜蓿碳、氮、磷、钾两年的矿化率分别为88.91%、94.45%、84.12%、99.72%,草木樨碳、氮、磷、钾两年的矿化率分别为88.94%、85.52%、83.15%、99.82%。
     玉米苜蓿、玉米草木樨间种轮作可以提高土壤有机质的含量,各个处理土壤有机质增加最多的是玉米草木樨3:1间种轮作。各个处理土壤速效氮变化大致呈现出在玉米生长期缓慢增加,玉米收获后至第二年春播时再逐渐升高的趋势,各个处理土壤速效氮含量差异显著,含量最高、增幅最大的是玉米苜蓿2:1处理,含量达118.0 mg/kg,增加了19.8mg/kg。各个处理速效磷含量与速效氮含量变化基本一致,均高于对照,差异显著,玉米苜蓿1:1处理土壤速效磷含量最高、增幅最大,含量达35.5 mg/kg,增加了10.1mg/kg。绿肥翻压后在玉米整个生长过程中土壤速效钾含量普遍快速升高,而经过冬季后增加不明显,与试验开始时相比,各个处理土壤中速效钾含量均增加明显,增加最高的是玉米草木樨1:1处理,达206 mg/kg,增幅最大的是玉米苜蓿3:1处理最大,达55.6mg/kg,增幅37.0%。
     玉米苜蓿、玉米草木樨间种轮作玉米的生育状况明显改善、单产显著提高,玉米、苜蓿间种比例从小到大单产依次提高47.1%、33.5%和23.3%,玉米、草木樨间种比例从小到大单产依次提高38.5%、26.6%和22.1%。
Alfalfa and sweet clover are the main green manure and forage grass crops in the Northeast. The purpose of study made sure that the decomposition regularity of alfalfa and sweet clover after turning over and the effect of soil fertility and maize yield as green manure after turning over. Development of major grain producing areas in the Northeast green manure crops to provide technical and theoretical support.
     The field tests and the indoor stimulation experiments were carried out in Administration of Agriculture Sideline Production Site of Fuyu Directly under the Regional Military Command of Shenyang of Fuyu county in Heilongjiang Province from 2008 to 2010.
     The decomposition regulation of dry matter and the mineralization regulation of N, P and K of alfalfa and sweet clover after turning over have the same tendency. The decomposition rate is proportional to temperture, so the fastest times between July and August. The K mineralization rate of two green manures were more than 96% in the first year. The dry matter decomposition of alfalfa and sweet clover were 87.54%,90.18% in two years, and C N P and K mineralization rate of alfalfa were 88.91%,94.45%,84.12% and 99.72% in two years, C N P and K mineralization rate of sweet clover were 88.94%,85.52%,83.15% and 99.82% in two years, respectively.
     Corn alfalfa and sweet clover rotation between the species which can increase soil organic matter content of treatment and improve the most is between 3:1 kind of corn sweet clover rotation. Changes in soil available nitrogen in all treatment generally showed slow increasing in the corn growing season, and after corn harvest until the second year spring had gradually increasing trendency. Each experiment with soil available nitrogen content was significantly different, and corn and alfalfa 2:1 treatment was higher than others,118.0mg/kg,and the largest increasing was corn and alfalfa 2:1 treatment,19.8mg/kg. Each experiment with Available phosphorus content had significant difference with CK and in basically the same with available nitrogen. The soil available phosphorus content of corn and alfalfa 1:1 treatment was higher than others,35.5mg/kg, and the largest increasing was corn and alfalfa 1:1 treatment, 10.1mg/kg.After turning over green manure, the available K content was generally fast in the whole growth, but had no significant increasing through the winter. Compared with the start of the trial, the available K content of each treatment were increased significantly, corn and sweet clover 1:1 treatment was higher than others, 206mg/kg, corn and alfalfa 3:1 was the largest of which 55.6 mg/kg, an increase of 37.0%.
     The intercropping of maize and green manure had a significant improvement in the growth and average per unit status of maize. The order of intercropping maize and alfalfa yield was 47.1%, 33.5% and 23.3%, and the order of intercropping maize and sweet clover yield was 38.5%,26.6% and 22.1% according to the width proportion from small to large.
引文
[1]陈礼智,王隽英.绿肥对土壤有机质影响的研究[J].土壤通报,1987(6):270-273
    [2]陈礼智.绿肥的种植和利用[M].土壤肥料,安徽科学技术出版社,1987:29-38
    [3]陈志鸿,胡勇军,郭继勋.生物、化学改良对重度盐碱化草地土壤水分特征影响的比较研究[J].东北师大学报,2002,34(3):92-97
    [4]董晓霞,郭洪海,孔令安.滨海盐渍地种植紫花苜蓿对土壤盐分特性和肥力的影响[J].山东农业科学,2001,1:24-25
    [5]方珊清,孙时银,汪雪薇.发展绿肥生产是生态农业建设的有效措施[J].安徽农学通报,2004,10(2):68
    [6]关连珠,张伯泉,颜丽等.有机肥料配施化肥对土壤有机质组分及生物活性影响的研究[J].土壤通报,1990,21(4):180-184
    [7]郭继勋,马文明,张贵福.东北盐碱化羊草草地生物治理研究[J].植物生态学报,1996,20(5):478-484
    [8]韩贵清,杨林章.东北黑土资源利用现状及发展战略[M].中国大地出版社,2009:30-39
    [9]何念祖,林咸永,林荣新等.面施和深施对秸秆中氮磷钾释放的影响[J].土壤通报,1995,26(7):40-42
    [10]贺志一.水稻土中各种有机物的分解过程[J].土壤学进展,1991,19(6):34-39
    [11]胡霭堂.植物营养学(下册).北京:中国农业大学出版社,2003:192
    [12]李逢雨.秸秆还田养分释放规律及稻草化感作用研究[D].四川:四川农业大学,2007,13-14
    [13]李建东,郑惠莹.松嫩平原盐碱化草地改良治理的研究[J].东北师大学报,1995,27(1):110-115
    [14]李新举,张志国,李贻学.土壤深度对还田桔秆腐解速度的影响[J].土壤学报,2001,38(1):135-138
    [15]李银平,徐文修,李钦钦等.绿肥压青对棉田土壤肥力的影响[J].新疆农业科学,2009,46(2):262-265
    [16]李月芬,汤洁.黄花草木樨改良盐碱土的试验研究[J].水土保持通报,2004,24(1):8-11
    [17]李宗新,董树亭,胡昌浩等.有机无机肥互作对玉米产量及耕层土壤特性的影响[J].玉米科学,2004,(3):100-202
    [18]刘国顺,罗贞宝,王岩等.绿肥翻压对烟田土壤理化性状及土壤微生物量的影响[J].水土保持学报,2006,20(1):95-98
    [19]鲁如坤.土壤农业化学分析方法[M].北京:中国农业科技出版社,1999:44-52
    [20]罗新义,曲善民,尤海洋.黑龙江省牧草种质资源的研究及其开发利用[J].黑龙江畜牧兽医,2006(9):64-66
    [21]史吉平,张夫道,林葆.长期定位施肥对土壤腐殖质结合形态的影响[J].土壤肥料,2002(6):8-12
    [22]孙聪姝,王宏燕,王兆荣等.长期培肥定位试验耗竭阶段各培肥物质对土壤有机质持续效应 的研究[J].东北农业大学学报,1998,29(1):11-12
    [23]汤洁,李月芬,林年丰等.应用生物技术改良退化土壤的效果—以黄花草木樨改良盐碱化土壤为例[J].生态环境,2004年,13(1):51-53
    [24]田慧梅,季尚宁.玉米草木樨间作效应分析[J].东北农业大学学报,1997,28(1):15-22
    [25]汪仁,张保烈,邱卫文.绿肥配施化肥对土壤养分含量和小麦产量的影响[J].辽宁农业科学,1994,3:9-12
    [26]王东升,徐志强,杜立宇等.大豆和小麦对矿物钾的活化作用研究[J].土壤通报,2006,17(6):1118-1122
    [27]王鹤桥,宿庆瑞,王英等.黑土区玉米带粮草间种的合理结构与综合效益[A].绿肥在持续农业中的地位和作用[C].沈阳:辽宁大学出版社,1992,161-164
    [28]王鹤桥.黑龙江绿肥牧草品种志[M].黑龙江出版总社,1985:30-46
    [29]王萍,殷立娟,李建东.松嫩平原盐碱化草地羊草的生长适应性及耐盐生理特性的研究[J].生态学报,1994,14(3):306-311
    [30]王文山,王维敏,张镜清.农作物残体在北京农田土壤中的分解[J].土壤通报,1989,20(3):113-115
    [31]王允青,郭熙盛.不同还田方式作物秸秆腐解特征研究[J].安徽农业科学,2006,34(10):2218-2220
    [32]温明霞,林德枝,易时来等.秸秆在土壤中的养分释放动态研究[J].西南农业学报,2004,17:276-278
    [33]谢瑾岚,龙桂芝.丘陵红壤桔园绿肥覆盖改土效应研究[J].湖南农业科学,1990(5):38-40
    [34]徐国伟,常二华,蔡建.秸秆还田的效应及影响因素[J].耕作与栽培,2005,1:6-9
    [35]薛瑞忠,白月善.草木樨的栽培及利用技术[J].内蒙古农业科技,2004(S2):111
    [36]杨首乐.潮土中小麦秸秆腐解残留率测定方法比较[J].河南农业科学,2005,12:60-63
    [37]张登辉,朱凤华,樊锦春.江苏沿海农区种植绿肥的不同耕作方式及其综合效益研究[A].绿肥在持续农业中的地位和作用[C].沈阳:辽宁大学出版社,1992:152-155
    [38]张电学,韩志卿,刘微等.不同促腐条件下秸秆直接还田对土壤酶活性动态变化的影响[J].土壤通报,2006,37(3):475-478
    [39]张景略,徐本生.土壤肥料学[M].河南科学技术出版社,1993:22-32
    [40]张镜清.14C、15N双标记田菁及玉米秸腐解试验[J].土壤通报,1984,15(1):37-38
    [41]张淑珍,孙传芳.绿肥品种资源研究[J].作物品种资源,1995(1):7-11
    [42]张翔,朱洪勋.长期施肥对土壤微生物和腐殖质组分的影响[J].华北农学报,1998,13(2):87-92
    [43]张友金.稻肥轮作对青紫泥土壤有机质积累的影响[A].绿肥在持续农业中的地位和作用[C].沈阳:辽宁大学出版社,1992:260-262
    [44]郑德明,姜益娟,吕双庆等.干旱地区有机肥料腐解及腐殖化系数的研究[J].土壤肥料,2004(2):15-19
    [45]郑元红,潘国元,毛国军等.不同绿肥间套作方式对培肥地力的影响[J].贵州农业科学,2009,37(1):79-81
    [46]周开芳,何炎.豆科冬绿肥翻压对土壤肥力和杂交玉米产量及品质的影响[J].贵州农业科学, 2003,31(增刊):42
    [47]朱祖徉.从绿肥的起爆效应探讨它的肥效机制及其在施用上的若干问题[J].浙江农业科学,1963(3):104-109
    [48]A.D.麦克拉伦,(闺九康译).土壤生物化学[M].农业出版社,1984:2-24
    [49]Appelt H,Coleman N.T and Pratt P 1975:Interation between arganic compounds,minerals and ions in volcanic-ash-derived soils:I.Adsorption of benzoate, P-OHbenzoate, salicyla teand phthalateions[J].Soil.Sci.Am.Proc,39:623-627
    [50]Earl K.D,Syers J.K. and Mclaughlin J.R,1979:Orgin of the effects of tartrate and acetate on phosphste sorption by soil and synthetic gels[J].Soil.Sci.Soc.Am.J,43:674-678
    [51]F.E.Allison绿肥的肥效[M].土壤农化,1977,4
    [52]Meek B.D,Graham L.E,Donovan T.J.and Mayberry K.S,1979:Phoshorus availability in a calcareous soil after high loading rate of animal manure[J].Soil.Sci.Soc.Am.J,43:741-743
    [53]Zhang Y.S,Wemer W and Sun X,1993:Phosphorus adsorption and desorplion in paddy soils as affected by organic manure and cellulose[J].Agribiol,Res,46:286-294

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700