黄土高原旱作农田水肥效应差异研究
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摘要
以黄土高原旱作区22年的长期定位试验为对照,开展了与长期定位试验相对应的大田对比试验,研究了施肥对土壤肥力以及硝态氮淋溶累积的影响,分析了不同施肥对小麦产量、构成因子和水肥利用率的影响,以及小麦不同生育期养分吸收、运移和累积过程,找出大田对比试验与长期定位试验的异同,为合理施肥提供参考。
     研究结果表明:长期定位试验中施用有机肥能够明显增加土壤养分,氮磷有机肥配施效果显著,化肥单施效果不及肥料配施;大田试验地基础肥力较1984年明显增加,表现在有机质、全氮和全磷分别提高了27.1%、84.2%和34.8%,有效氮、有效磷和速效钾增加了46.9%、540.0%和10.2%,养分水平与长期定位试验中氮磷(N120P60)配施处理相近。长期定位试验中氮磷配施或与有机肥配施能够有效地减少土壤中硝酸盐的淋溶和累积,氮肥单施硝态氮淋溶程度增强,且累积量最大,大田对比试验地硝态氮总累积量较长期定位试验中施用氮肥的总累积量少。长期施用有机肥土壤0-3m储水量较对照明显减少,土壤出现了生物利用性干层,大田对比试验地的储水量与长期定位试验中不施肥的储水量差异不明显。当前大田施肥既能培肥土壤,提高养分含量,又能减少硝态氮累积,且储水量较高,因此大田生态系统尚处在一个良性循环状况。
     大田对比试验中磷肥有机肥配施能提高成穗数,单施磷肥千粒重增加,长期定位试验中磷肥单施或与有机肥配施有利于穗粒数和千粒重的提高。两试验中氮磷配施的小麦产量较其对照分别增高了21.5%和111.7%,交互作用明显,增产效果显著;但是,大田对比试验各处理的产量均高于长期定位试验,增加幅度为2103.4-3316.5kg/hm2,单施磷肥差异最大,大田对比试验较长期定位试验增加了334.6%。氮磷配施的肥料贡献率最高,同时又是提高氮、磷肥效的最佳途径,长期定位试验的肥料贡献率和平均肥效较大田对比试验均有提高。两试验中氮磷配施的水分利用率分别提高了24.1%和95.2%,大田对比试验各处理的水分利用率较长期定位试验增加了46.5-290.0%。两试验中氮肥单施、磷肥配施的肥料利用率较其它处理的高,大田对比试验中氮、磷肥利用率普遍较低。
     两试验中植株的氮、磷累积量变化趋势相似,各器官的氮素和磷素均从茎、叶逐渐向穗、籽粒转移,后期钾素的分配主要集中在茎、叶中,籽粒形成阶段出现亏损;长期定位试验中施用有机肥处理的氮、磷、钾累积量较大,长期单施磷肥和不施肥,植株养分累积量不及大田对比试验。
     两试验中小麦干物质累积均随生育期的进程呈增加趋势,拔节期至孕穗期干物质积累量较大,随后有所降低;长期定位试验中有机肥与化肥配施效果明显,成熟期氮磷配施的干物质量较对照增加了27.2%,累积量最高;大田对比试验的干物质累积量较长期定位试验均有增加,氮、磷单施和对照差异较大。
     不同施肥的P收获指数最高,N收获指数次之,K收获指数最低;大田对比试验中氮磷配施效果明显,氮磷有机肥配施K收获指数最高,长期定位试验中有机肥和氮肥单施有利于N、P收获指数的提高,氮磷配施的K收获指数最高;大田对比试验的养分收获指数较长期定位试验有不同程度的提高,氮磷有机肥配施差异明显。
Compared with 22 years long-term experiment of applying fertilizers on continuous wheat, This experiment studied the difference between the effect of field comparison experiment and long-term experiment on soil nutrient fertility and Nitrate accumulation, the effects of different fertilizing on yield、water use efficiency、fertilizer use efficiency and nutrient absorption were analyzed, to keep agriculture sustainable developing.
     The result showed that long term application of manure could increase soil nutrient, combination applying of NP and manure was significant, combination fertilizer application was better than single applying N or P. The soil nutrient content of field comparison experiment increased obviously, organic matter、total N and total P increased respectively by 27.1%、84.2% and 34.8%,available N、P and K increased respectively by 46.9%、540.0% and 10.2%,the soil fertility level was close to NP treatment. Combination applying of N and P or manure can reduce nitrate accumulation, the nitrate accumulation was highest with single applying N, and the nitrate accumulation in field comparison experiment was fewer than of which long term application of N in long term experiment. The pondage reduced obviously with Long term application of manure, but there was no clear difference when pondage in field comparison experiment compared with Control in long term experiment. On current, field fertilizing not only could increase soil nutrient, but also reduce nitrate accumulation, and the pondage was higher, so ecosystem is still at good situation.
     In field comparison experiment, wheat’sear numbers increased with Combination applying of manure and chemical fertilizer, and the weight of thousand-grain improved with single applying P, single applying P.or combination applying M could increase grain and weight of thousand-grain in long term experiment. The yield increased by 21.5% and 111.7% with Combination applying of N and P in two experiments, and the interaction of N and P was good; Comparing with long term experiment, the yield in field comparison experiment increased by 2103.4 kg/hm2 to 3316.5kg/hm2, especially in P treatment, the yield increased by 334.6%. Combination applying of N and P could not only improve the contribution ratio of fertilizer to yield but also improve efficiency of N、P, the contribution ratio of fertilizer to yield in comparison experiment was better than which in long term experiment.The WUE increased respectively by 24.1% and 95.2% in NP treatment in two experiment; Comparing with long term experiment, the WUE in field comparison experiment increased by 46.5% to 290.0%. The FUE increased with single applying N and combination applying of P, but the FUE was generally lower in field comparison experiment.
     The change of N,P accumulation in plants was similar to each other ,N、P in each organs transferred from stems and leaves to ears or grains, the K accumulation was higher in stems and leaves, and there was obviously decreased in maturation stage. The N,P accumulation was higher in application of manure treatment, was lower in long term experiment in P and Control.
     Wheat’s dry matter accumulation increased with stage’s change in two experiments, and there was a high accumulation at elongation and booting. Combination applying of manure and chemical fertilizer could increase dry matter accumulation sharply, and dry matter accumulation improved by 27.2% in NP treatment at Maturation in long term experiment, comparing with long term experiment, dry matter accumulation in field comparison experiment was higher, the difference of N, P and Control was great.
     The P harvest index was higher than N harvest index, K harvest index was lowest with applying fertilizer in dry land. In comparison experiment, combination applying of N and P could improved nutrient harvest index, K harvest index was highest in NPM treatment; In long term experiment, single applying of manure and N was benefit to improve N, P harvest index, K harvest index was highest in NP treatment. At certain extent, nutrient harvest index in comparison experiment was higher than which in long term experiment, the difference of NPM was great.
引文
[1]李秧秧.无机营养提高作物抗旱性的生理基础[A].山仑,陈培元.旱地农业生理生态基 [C].北京:科学出版社,1998:222-232.
    [2]魏孝荣,郝明德,张春霞等.黄土区长期定位培肥试验对土壤肥力的影响[J].水土保持研究,2003,10(1):37-39.
    [3]郭胜利,张文菊,党廷辉等.干旱半干旱地区农田土壤NO3-N深层积累及其影响因素[J].地球科学进展,2003,18(4):585-591.
    [4]党廷辉,郭胜利,郝明德.黄土旱塬长期施肥下硝态氮深层累积的定量研究[J].水土保持研究, 2003,11(3):58-60.
    [5]魏孝荣,郝明德,张春霞等.旱地长期施肥对土壤水分的影响[J].水土保持研究,2003,10(1):95-97.
    [6]黄明斌,杨新民,李玉山.黄土高原生物利用型土壤干层的水文生态效应研究[J].中国生态农业学报,2003,11(3):113-116.
    [7]文宏达,刘玉柱,李晓丽等.水肥耦合与旱地农业持续发展[J].土壤与环境,2002,11(3):315-318.
    [8]梁运江,依艳丽,许广波等.水肥耦合效应的研究进展与展望[J].湖北农业科学,2006,45(3)385-388.
    [9]汪德水,程宪国,张美荣等.旱地土壤中的肥水激励机制[A].汪德水.旱地农田肥水关系原理与调控技术[C].北京:中国农业科技出版社,1995:195-203.
    [10]于亚军,李军,贾志宽等.旱作农田水肥耦合研究进展[J].干旱地区农业研究,2005,23(3):220-224.
    [11]汪德水.旱地农田肥水关系原理与调控技术[M].北京:中国农业出版社,1995.
    [12]Viets FG.Water deficits and nutrient availability [A].Kozlowski T T.water deficits and plant growth[C].USA:Acad Press,1972,2l7-247.
    [13]Arnon.Physiological principles of dryarglana crop production[A].In Gupta,US.physiological aspects of dry land farming[C].New York:Universal Press,1975,3-124.
    [14]Lahiri A.N, Singh S,Kackar N.L. Studies on plant water relationships. VI. Influence of nitrogen level on performance and nitrogen content of plant under drought[J].Proceedings of the Indian National Science Academy,1973, 39:77–90.
    [15]Bhan S,Misra F.K.Effects of variety,spacing and soil fertility on root development in groundnut tinder arid conditions[J].Indian,J.Agric.Sci,1970,(40):1050-1055.
    [16]党廷辉,彭琳,戴鸣钧等.旱塬长期施肥的产量效应与土壤肥力演变[J].水土保持学报,1995,9(1):55-63.
    [17]沈善敏.中国土壤肥力[M].北京:中国农业出版社,1998.
    [18]李忠佩,唐永良,石华等.不同施肥制度下红壤稻田的养分循环与平衡规律[J].中国农业科学,1998,31(1):46-54.
    [19]张璐,沈善敏,宇万太.辽西褐土施肥及养分循环再利用中长期试验Ⅱ.土壤养分收支[J].土壤与环境,2001,10(1):51-54.
    [20]刘鸿翔,王德禄,王守字等.黑土长期施肥及养分循环再利用的作物产量及土壤肥力质量变化Ⅲ.土壤养分收支[J].应用生态学报,2002,13(11):1410-1412.
    [21]宇万太,张璐,殷秀岩等.下辽河平原农业生态系统不同施肥制度土壤养分收支[J].应用生态学报,2002,13(12):1571-1574.
    [22]Lombin G.The effects of continuous fertilization on nutrient balance and crop yield in the northern Nigerian savannah:a preliminary assessment [using maize][J].Can.J.Soil. Sci.,1981,61(1):55-56.
    [23]李贵华.不同施肥条件下灰漠土肥力的变异与肥效的研究[J].土壤肥料,1994,(5):1-4.
    [24]杨靖.洛桑试验站150周年经典试验的研究进展[J].土壤学进展,1995,23(1):9-12.
    [25]陈琼贤,刘国坚,段炳源等.有机无机肥料对土壤肥力和作物产量的影响研究初报[J].热带亚热带土壤科学,1996,5(1):7-13.
    [26]姚源喜,杨延蕃,刘树堂等.长期定位施肥对作物产量和土壤肥力的影响[J].莱阳农学院学报,1991,8(4):245-251.
    [27]党萍莉,马旭华,张一平等.不同施肥条件对楼土有机无机复合状况的影响[J].土壤肥料,1994,(3):1-3.
    [28]Govi M,Francioso O,Ciavatta C et a1.Influence of long-term residue and fertilizer applications on soil humic substances:A study by electro focusing[J].Soil Sci,1992,154(1):8-13.
    [29]Sommerfeldt TG,Chang C,Entz T.Long.term annual applications increase soil organic matter and nitrogen and decrease carbon to nitrogen ratio[J].Soil Sci.Soc.Amer.J,1988,52(6):1668-1672.
    [30]关焱,宇万太,李建东.长期施肥对土壤养分库的影响[J].生态学杂志,2004,23(6):131-137.
    [31]张夫道.长期施肥条件下土壤养分的动态和平衡Ⅱ.对土壤氮的有效性和腐殖质氮组成的影响[J].植物营养与肥料学报,1996,2(1):39-48.
    [32]林葆,林继雄,李家康.长期施肥的作物产量和土壤肥力的变化[J].植物营养与肥料学报,试刊,1994,(1):6-18.
    [33]梁国庆,林葆,林继雄等.长期施肥对石灰性潮土氮素形态的影响[J].植物营养与肥料学报,2000,6(1):3-1O.
    [34]黄东迈.有机肥无机肥对提高土壤氮素肥力的作用及其配合施用[A].我国土壤氮索研究工作的现状与展望[C].北京:科学出版社,1986,92-103.
    [35]程丽丽,文启孝,施书莲.有机肥和化学肥配合施用时氮素的供应和转化[A].我国土壤氮素研究工作的现状与展望[C].北京:科学出版社,1986,104-115.
    [36]Mercik S,Nemeth K.Effects of 60 year N,P,K and Ca fertilization on EUF nutrient fractions in the soil and on yields of rye and potato crops[J].Plant Soil,1985,83(1):151-159.
    [37]Rasmussen PE,Rohde CR.Long—term tillage and nitrogen fertilization effects on organic nitrogen and carbon in semiarid soil [J].Soil Sci.Soc.Amer.J,1988,52(4):l114-l117.
    [38]刘杏兰,高宗,刘存寿等.有机、无机肥配施的增产效应及对土壤肥力影响的定位研究[J].土壤学报,1996,33(2):138-147.
    [39]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.
    [40]劳秀荣,孙伟红,王真等.秸秆还田与化肥配合施用对土壤肥力的影响[J].土壤学报,2003,40(4):618-622.
    [41]崔文华,卢亚东.化肥和有机肥对作物产量和土壤养分影响的研究[J].土壤通报,1993,24(6):271-272.
    [42]孙聪姝,王兆荣,金明花等.长期培肥定位试验耗竭阶段各培肥物质对土壤氮库持续效应的研究[J].东北农业大学学报,1998,29(3):209-218.
    [43]郑铁军.黑土长期施肥对土壤磷的影响[J].土壤肥料,1998,(1):39-41.
    [44]顾益初,钦绳武.长期施用磷肥条件下潮土磷素的积累、形态转化和有效性[J].土壤,1997,29(1):13-17.
    [45]Bolland MDA,Weatherley AJ,Gilkes.The long—term residual value of rock phosphate and super phosphate fertilizers for various plant species under field conditions[J].Fert.Res.,1989,20(2):89-100.
    [46]周广业,阎龙翔.长期施用不同肥料对土壤磷素形态转化的影响[J].土壤学报,1993,30(4):443-446.
    [47]Swarup A,Chhillar RK. Build up and depletion of soil phosphorus and potassium and their uptake by rice and wheat in a long—term field experiment[J].Plant Soil,1986,91(2):161-170.
    [48]Wang Huo-Yan.Zhou Jian-Min.CHEN Xiao-Qin et a1.Interaction of NPK fertilizers during their transformation in soils:Ⅲ.Transformations of monocalcium phosphate[J].pedosphere,2004,14(3):379-385.
    [49]雷永振,丘卫文,王祥珍等.玉米钾肥长期定位试验作物产量和土壤钾素的变化[J].辽宁农业科学,2003,(4):1-3.
    [50]刘荣乐,金继运,吴荣贵等.我国北方土壤.作物系统内钾素循环特征及秸秆还田与施钾肥的影响[J].植物营养与肥料学报,2000,6(2):123-132.
    [51]周晓芬,张彦才,步丰骥.河北省主要农业土壤有机肥料对土壤钾素的贡献[J].河北农业科学,1997,1(2):21-24.
    [52]索东让,侯格平,王平.定位连施土粪对土壤钾的影响[J].土壤肥料,2002,(2):36-38.
    [53]沈善敏.长期土壤肥力试验的科学价值[J].植物营养与肥料学报,1995(1)3:1-9.
    [54]鲁如坤等著.土壤一植物营养学原理和施肥[M].北京:化学工业出版社,1989.
    [55]李世清,李生秀.半干旱地区农田生态系统中硝态氮的淋失[J].应用生态学报,2000,11(2):240-242.
    [56]郭胜利,党廷辉,郝明德.施肥对半干旱地区小麦产量、N03一一N累积和水分平衡的影响[J].中国农业科学,2005,38(4):754-760.
    [57]郭胜利,周印东,张文菊等.长期施用化肥对粮食生产和土壤质量形状的影响[J].水土保持研究,2003,10(1):16-22.
    [58]李迎春,彭正萍,薛世川等.磷、钾对冬小麦养分吸收、分配及运转规律的影响[J].河北农业大学学报,2006,29(5):1-6.
    [59]韩燕来,介晓磊,谭金芳等.超高产冬小麦氮磷钾吸收、分配与运转规律的研究[J].作物学报,1998,24(6):908-915.
    [60]张会民,刘红霞,苗艳芳等.施钾对旱地冬小麦养分含量及吸收量的影响[J].干旱地区农业研究,2002,20(4):34-37,25.
    [61]胡田田,刘翠英,李岗等.施肥对土壤供肥和冬小麦养分吸收及其产量的影响[J].干旱地区农业研究,2001,(19):36-41.
    [62]胡田田,李岗,韩思明.旱地冬小麦吸收氮、磷的营养特征[J].西北植物学报,2000,20(5):826—830.
    [63]Papakosta D K,Gagianas A A.Nitrogen and dry matter accumulation,remobilization,and losses for Mediterranean wheat during grain filling[J].Agron,J,1991,83:864-879.
    [64]Singh G. Relationship between growth in dry weight and uptake of nitrogen and phosphorus in wheat plant [J]. Soi1 Sci,1972,94:331-333.
    [65]Batwrighto G O,Haas H J.Development and composition of spring wheat as influenced by nitrogen and phosphorus fertilization[J].Agroa.J,1961,53:33-36.
    [66]Rumburg C R.Accumulation and loss of nitrogen during growth and maturation of cereal rye(scale cereals)[J].Agron.J,1970,62:311—313.
    [67]Gasser J K R, Thorburn M A P. Growth composition and nutrient uptake of spring wheat:effects of fertilizer N irrigation and CCC on dry matter and N,P,K,Ca,Mg and Na [J].J,Agric,sci.,1972 ,78:393-404.
    [68]钦绳武,顾益初,朱兆良.潮土肥力演变与施肥作用的长期定位试验初报[J].土壤学报, 1998,35:367-375.
    [69]李玉山,张孝忠,郭明航等.黄土高原南部作物水肥产量效应的田间研究[J].土壤学报,1990,27(1):1-7.
    [70]郝明德,王旭刚,党廷辉等.黄土高原旱地小麦多年定位施用化肥的产量效应分析[J].作物学报,2004,30:1108-1112.
    [71]蔡祖聪,钦绳武.作物N、P、K含量对于平衡施肥的诊断意义[J].植物营养与肥料学报,2006, 3:1-7.
    [72]刘鸿翔,王德禄,王守字等.黑土长期施肥及养分循环再利用的作物产量及土壤肥力质量变化Ⅲ.土壤养分收支[J].应用生态学报,2002,13(11):1410-1412.
    [73]程宪国,汪德水,张美荣等.不同土壤水分条件对冬小麦及养分吸收的影响[J].中国农业科学,1996,29(4):7I-74.
    [74]杨建昌,王志琴,朱庆森.不同土壤水分状况下氮素营养对水稻产量的影响及其生理机制的研究[J].中国农业科学,1996,29(4):58-66.
    [75]党廷辉,高长青,彭琳等.长武旱塬轮作与肥料长期定位试验[J].水土保持研究,2003,10(1):61-64.
    [76]刘一.施肥对黄土高原旱地冬小麦产量及土壤肥力的影响[J].水土保持研究,2003,10(1):40-42.
    [77]张凤翔,周明耀,徐华平等.水肥耦合对冬小麦生长和产量的影响[J].水利与建筑工程学报,2006,3(2):22-24.
    [78]山仑.提高半干旱地区农田生产力的现实途径和未来策略[A].中国科学院西北水土保持研究所集刊[C],1988,8:1-9.
    [79]关军锋,李广敏.干旱条件下施肥效应及其作用机理[J].中国生态农业学报,2002,10(1):59-60.
    [80]上官周平.周维.栽培条件对冬小麦叶片水分利用率的影响植物[J].营养与肥料学报,1998,4(3):231-236.
    [81]Zeng Qiu-peng,Patrick H BROWN.Soil potassium mobility and uptake by corn under differential soil moisture regimes[J].Plant and Soil,2000,221:121-134.
    [82]汪德水.旱地农田肥水协同效应与耦合模式[M].北京:气象出版社,1999.
    [83]赵立新,荆家海.旱地冬小麦施肥效应研究[J].干旱地区农业研究,1991,(4):46-51.
    [84]樊廷录.提高黄土高原旱地抗逆减灾能力的肥定位试验研究[J].水土保持研究,2003,10(1):6-8.
    [85]穆兴民.水肥耦合效应与协同管理[M].北京:中国林业出版社,l999.
    [86]张仁陟,李小刚,胡恒觉.施肥对提高旱地农田水分利用效率的机理[J].植物营养与肥料学报,1995,5(3):221-226.
    [87]山仑,陈培元.旱地农业生理生态基础[M].北京:科学出版社,1998.
    [88]党廷辉.施肥对旱地冬小麦水分利用效率的影响[J].生态农业研究,1999,7(2):28-31.
    [89]樊军,郝明德,党廷辉.旱地长期定位施肥对冬麦水分利用的影响研究[J].土壤,2000,6:315-318,322.
    [90]郝明德,李军超,党廷辉.长武试验示范区高效农业生态经济系统研究[J].水土保持研究,2003,10(1):1-5.
    [91]赵聚宝,梅旭荣.晋东南地区旱地农田土壤水分状况及水分循环特征[J].中国农业科学,1992,25(6):l-8.
    [92]吕家珑,张保军,李松龄等.施肥对早地冬小麦水分利用率和产量的影响[J].西北林学院学报,1998,13(2):56-60.
    [93]王邦锡,黄久常,赵大千等.旱地施肥对春小麦产量和水分利用效率影响的研究[J].干旱地区农业研究,1990,(4):98-104.
    [94]郝明德,来璐,王改玲等,黄土高原塬区长期施肥对小麦产量的影响[J].应用生态学报,2003,14(11):1893-1896.
    [95]樊军,郝明德,党廷辉.旱地长期定位施肥对土壤剖面硝态氮分布与累积的影响[J].土壤与环境,2000,9(1):23-26.
    [96]郭胜利,党廷辉,郝明德.黄土高原沟壑区不同施肥条件下土壤剖面中矿质氮的分布特征[J].干旱地区农业研究,2000,18(1):22-27.
    [97]史吉平,张夫道,林葆.长期施用氮磷钾化肥和有机肥对土壤氮磷钾养分的影响[J].土壤肥料,1998(1):7-10.
    [98]党廷辉.郭胜利.樊 军.郝明德。长期施肥条件下黄土旱塬土壤NO3--N的淋溶分布规律[J].应用生态学报,2003,4(8):1265-1268.
    [99]郝明德,姚振镐,韩贵杰等.渭北旱塬地区粮食作物优化施肥模式的研究[M].西安:科学技术文献出版社,1991.
    [100]李玉山.渭北旱塬土壤水分动态规律及对小麦生长关系[J].陕西农业科学,1982,(2):1-5.
    [101]李玉山.长武王东沟高效生态经济系统综合研究[M].北京:科学技术文献出版社,1991.
    [102]江云,马友华,陈伟等.作物水分利用率的影响因素及其提高途径探讨[J].中国农学通报,2007,23(9):269-273.
    [103]吴大付,杨文平.提高作物水分利用率的探讨[J].河南科技学院学报(自然科学版),2005,33(2),1-3.
    [104]吴国梁,崔秀珍.高产小麦氮磷钾营养机理和需肥规率研究[J].中国农学通报,2000,16(2):8-11.
    [105]张鸿程,黄甫湘荣,宝德俊等.冬小麦地上部分器官氮磷钾的累积分配和运转的研究[J].土壤通报,2000,31(4):177-179
    [106]张少民,郝明德,柳燕兰.黄土区长期施用磷肥对冬小麦产量、吸氮特性及土壤肥力的影响.西北农林科技大学(自然科学版),2007,35(7):159-163.
    [107]卢良恕.中国小麦栽培研究新进展[M].北京:农业出版社,1993.
    [108]粱振兴,刘兴海.小麦产量形成的栽培技术原理[M].北京:北京农业大学出版社,1994.
    [109]Daigger L A,Sander D H,Peterson G A.Nitrogen content of winter wheat during growth and maturation[J].Agron J,1976,68:815-818.
    [110]Egera A T,AWSM van.Exudation of ninhydrinpositive compounds by pea-seedling roots:A study of the sites of exudation and of the composition of the exudates[J].Plant Soil,1975,42:37-47.
    [111] Farquhar G D,Wetselaar R,Firthp M.Ammonia volatilization from senescing leaves of maize[J].Science,1979,203:1257-1258.
    [112]田宵鸿.小麦和玉米生长过程中氨态氮素的挥发损失[D].陕西杨凌:西北农业大学,1992.
    [113]李生秀,常青,何琳.植物体氮素的挥发损失Ⅱ.植物收获期地上部分氮素减少与土壤、作物和肥料供应的关系[J].西北农业大学学报,1992,20(增刊):7-11.

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