生物炭与有机肥对风沙土根际养分含量及玉米生长的影响

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关键词:玉米(ZeamaysL.);风沙土;生物炭;有机肥;根际土壤;养分含量

中图分类号:S156.99;S513 文献标识码:A

文章编号:0439-8114(2026)01-0048-06

DOI:10.14088/j.cnki.issn0439-8114.2026.01.009 开放科学(资源服务)标识码(OSID):口

Effects of biochar and organic fertilizer on rhizosphere nutrient content and maize growth in aeoliansandysoil

SUN Bo-yan,WANG Yao-feng (College of Resources and Environment,Xinjiang Agricultural University,Urumqi 83oo52,China)

Abstract:Toinvestigatetheefectsofbiocharandorganicfertilizerapplicationotheimprovementofeoliansandysoil,astudywas conductedusingmaize(ZeamaysL)asthetestcrop,withpearbranch-derivedbiocharandchickenmanureorganicfertilizerasamendments.Nine treatments were established:CK(control,without biochar and organic fertilizer),biochar application (1,4,20t/hm2 ) organic fertilizerapplication (1,4,20t/hm2 ),and combined applications( 4t/hm2 biochar +4t/hm2 organic fertilizer, 4t/hm2 biochar t/hm²organic ferilizer).Thecontentsoforganiccarbon,alkali-hydrolyzablenitrogen,andavailablephosphorusinrhizosphersoil,andtearationcharacteristicsofplanthightstemameter,ndrootlngthatdierentgrowthsages(selingot ing,filling,heading,and maturity stages)were analyzed.The results showed that the applicationof biochar( 20t/hm2 )and organic fertilizer ( 20t/hm2 )significantly increased rhizosphere soil organic carbon content atthe seedling and heading stages,with increases of 28.79% and 36.21% ,respectively.The application of biochar and organic fertilizer promoted plant height,stem diameter,root length,andcelldifeintipaturatzoeacossallgothages.ealameerfts,ndber anddiameterofxylemveselsinthematurationzoneweresignificantlynhanced.Theresultsofcorelationanalysissowedhatbio charapplicationratewassignificantlypositivelycorelatedwithrhzospheresoilorganiccarbonandalkali-ydolyzablenitrogencontent ( P<0.05 ).Theapplicationamountoforganic fertilizer was significantlypositivelycorelated withavailablephosphorus content and corn stem diameter ( P<0.05 )

KeyWords:corn(Zeamays L.);aeoliansandysoil;biochar;organic fertilizer;rhizosphere soil;nutrientcontent

风沙土作为典型的沙质土壤,其形成主要受风蚀和风力沉积作用影响,在全球十旱、半干旱地区广泛分布。(剩余9747字)

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