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1、河北農(nóng)業(yè)大學(xué)博士學(xué)位論文河北省農(nóng)田土壤磷素轉(zhuǎn)化、平衡與產(chǎn)量效應(yīng)姓名:廖文華申請學(xué)位級(jí)別:博士專業(yè):土壤學(xué)指導(dǎo)教師:劉建玲20120526而施用有機(jī)肥還可增加土壤有機(jī)磷含量,而且無論增施磷肥或有機(jī)肥,有效磷占全磷的比重都有掰增嫻。7、連續(xù)8年定位施用不同用量的磷肥和有機(jī)肥增加了土壤磷素的積累量,土壤Ca2。P、Ca8.P、AI。P、Fe.P含量均顯著增加,而O。P、Calo.P含量變化不顯蔫。隨著磷肥和有機(jī)囂跫用量的增加,Ca2.P、Ca8,P無釩磷麴比重在逐漸增加,酉Fe.P、O—P、Cal0.P在逐漸降低。積累磷的有效
2、性比重逐漸增加,增施磷肥Ca2.P、Ca8。P、A1.P、Fe。P含量每年分別增加0。3.6.6、10。5.42.7、3.0。13.1和1.6。4.7mg·kg-l。8、長期的有機(jī)。無機(jī)肥配施試驗(yàn)表明,連續(xù)3年過量施用磷肥或有機(jī)肥,±壤0.60cm±壤有效磷顯著增加,施腿5年后,60,--一80cm土壤有效磷顯蔫增加,藤且高量施用磷舅墨和有飆鼴80.100cm±層有效磷明顯增翻,說明隧著施勰時(shí)間的延長,積累的磷索逐漸向下遷移。9、定位監(jiān)測不霹土層菜地土壤有效磷的變化結(jié)果:土壤磷素主要在表層_翕集,隨著磷肥用量和棚齡的增加
3、,積累磷素逐漸向深層遷移,其中60。80cm土層積累磷素占0.80cm土體總積累量的6。7%.11.9%。關(guān)鍵詞:磷素;農(nóng)田;蔬菜;果樹;磷素累積;遷移Transformation,BalanceandYieldResponseofSoilPhosphorusintheArableLandsinHebeiProvinceAuthor:UA0WrenhuaMajor:SoilscienceAdvisior:Prof.UUJianlingAbstractSafemanagementpracticesonthesoilphos
4、phorus(P)hasbeenhighlyconcernedbythepublicduetotheconsecutiveaccumulation,declingyieldresponseandincreasingenvironmentalriskcausedbytheexcessiveapplicationofPfertilizersintheagricultureinChina.Inthisstudy,theinput,balanceandspatio-tempeoralvariationofphosphorusin
5、thecontinuumoffertilizer-plant—soilduringthelast30yearswereinvestigatedfromliteratureatmacroscale,andthetransformationandavailabilityoftheaccumulatedPinsoilweremonitoredinsituduringlong—termexperiment.Theresultsobtainedatmacroandplotlevelwerecombinedtoindicatethe
6、changesoftotalPapplicationinHebeiprovinceaswellasthePbalance,yieldresponsetotheapplicationrateandformsofPfertilizers,transformationandmovementinthesoilprofileforthegrain,vegetableandorchardproductionsysteminHebei.Themainresultsareasfollowing:1.Itwasfoundthatthefa
7、stincreaseperiodsofPfertilizationrateinHebeiprovinceduring1980-1985and1990-1995wereobserved,wheretheaverageannualincreaseratewas14%;meanwhile,thetotalconsumptionofcompoundPfertilizersreachedupto894木103tonesandtherespectivecontributiontothetotalPconsumptionincreas
8、edfrom10%2.AnalysisofPbalancebasedontheinput—outputindicatedthatthesoilPstatusofwinterwheat—summermaizerotationsystemswerecharacterizedwithdepletionperiod(1949