河南农业大学学报
河南農業大學學報
하남농업대학학보
ACTA AGRICULTURAE UNIVERSITATIS HENANENSIS
2010年
1期
28-33
,共6页
王良桂%张焕朝%朱强根%蒋永丰%颜开义%王福好
王良桂%張煥朝%硃彊根%蔣永豐%顏開義%王福好
왕량계%장환조%주강근%장영봉%안개의%왕복호
杨树人工林%连栽代次%土壤矿质化%间歇淋洗法
楊樹人工林%連栽代次%土壤礦質化%間歇淋洗法
양수인공림%련재대차%토양광질화%간헐림세법
poplar plantation%successive rotation%soil mineralization%intermittent leaching
采用好气培养间歇淋洗的方法,研究了江苏苏北地区不同林龄(1代4年生林地、1代10年生林地)和连栽代次(1代4年生林地、2代4年生林地)的杨树人工林土壤及农田无林地土壤在20和30℃培养条件下氮素矿质化特性.结果表明,各样地土壤经4周培养的矿化量为36.70~95.63 mg·kg~(-1),平均矿化速率约为1.31~3.42 mg·kg~(-1)·d~(-1).林龄和连栽代次对杨树人工土壤的矿质化作用有明显的影响,其中主要是对硝化作用的影响,而对氨化作用影响不明显.与1代4年生林地相比,1代10年生林地土壤矿化累积量和硝化累积量分别降低了11%~17%和13%~20%;而2代4年生林地土壤则分别降低了39%~43%和45%~49%,显示连栽代次对土壤矿质化作用的影响更加明显.各样地土壤矿化速率和硝化速率在培养的第1周最高,然后随培养周期迅速降低;而氨化速率则是在第2周达到峰值,然后逐渐降低.随林龄和连栽代次的增加,土壤矿化速率和硝化减小,尤其是培养第1周,而氨化速率差异不显著.各样地30℃培养条件下的土壤矿化量和矿化速率均明显高于20℃,表明培养温度对土壤矿质化作用具有明显的影响.
採用好氣培養間歇淋洗的方法,研究瞭江囌囌北地區不同林齡(1代4年生林地、1代10年生林地)和連栽代次(1代4年生林地、2代4年生林地)的楊樹人工林土壤及農田無林地土壤在20和30℃培養條件下氮素礦質化特性.結果錶明,各樣地土壤經4週培養的礦化量為36.70~95.63 mg·kg~(-1),平均礦化速率約為1.31~3.42 mg·kg~(-1)·d~(-1).林齡和連栽代次對楊樹人工土壤的礦質化作用有明顯的影響,其中主要是對硝化作用的影響,而對氨化作用影響不明顯.與1代4年生林地相比,1代10年生林地土壤礦化纍積量和硝化纍積量分彆降低瞭11%~17%和13%~20%;而2代4年生林地土壤則分彆降低瞭39%~43%和45%~49%,顯示連栽代次對土壤礦質化作用的影響更加明顯.各樣地土壤礦化速率和硝化速率在培養的第1週最高,然後隨培養週期迅速降低;而氨化速率則是在第2週達到峰值,然後逐漸降低.隨林齡和連栽代次的增加,土壤礦化速率和硝化減小,尤其是培養第1週,而氨化速率差異不顯著.各樣地30℃培養條件下的土壤礦化量和礦化速率均明顯高于20℃,錶明培養溫度對土壤礦質化作用具有明顯的影響.
채용호기배양간헐림세적방법,연구료강소소북지구불동림령(1대4년생임지、1대10년생임지)화련재대차(1대4년생임지、2대4년생임지)적양수인공림토양급농전무임지토양재20화30℃배양조건하담소광질화특성.결과표명,각양지토양경4주배양적광화량위36.70~95.63 mg·kg~(-1),평균광화속솔약위1.31~3.42 mg·kg~(-1)·d~(-1).림령화련재대차대양수인공토양적광질화작용유명현적영향,기중주요시대초화작용적영향,이대안화작용영향불명현.여1대4년생임지상비,1대10년생임지토양광화루적량화초화루적량분별강저료11%~17%화13%~20%;이2대4년생임지토양칙분별강저료39%~43%화45%~49%,현시련재대차대토양광질화작용적영향경가명현.각양지토양광화속솔화초화속솔재배양적제1주최고,연후수배양주기신속강저;이안화속솔칙시재제2주체도봉치,연후축점강저.수림령화련재대차적증가,토양광화속솔화초화감소,우기시배양제1주,이안화속솔차이불현저.각양지30℃배양조건하적토양광화량화광화속솔균명현고우20℃,표명배양온도대토양광질화작용구유명현적영향.
By the aerobic incubation-intermittent leaching method (20and 30 ℃) ,the characteristics of soil nitrogen mineralization in different aged poplar plantation stands (the first rotation of four-year-old and ten-year-old) ,the different successive rotation poplar plantation stands (the first rotation of four-year-old and the second rotation of four-year-old) and the agricultural land were studied in Chen-wei Forest Farm,Sihong County,Jiangsu.The results showed that the cumulative mineralized N of soils from the four studied sites ranged from 36.70 t0 95.63 mg · kg~(-1) during 4 weeks incubation and the average mineralization rate of soils approximately ranged from 1.31 t0 3.42 mg · kg~(-1) · d~(-1).The stand ages and successive rotations had great effects on soil N mineralization (mainly on nitrification).Compared with the first rotation stands of 4-year-old poplar plantation,the cumulative mineralized N and nitrified N decreased by 11% ~17qo and by 13% ~20% ,respectively in the first rotation stands of 10-year-old poplar plantation,while in the second rotation stands of 4-year-old poplar plantation it decreased by 3g% ~43% and by 45% ~49% respectively.Soil mineralization rate and nitrification rate were the greatest in the first week and then sharply decreased in the following incubation weeks for all sites while the peak value of ammonification rate occurred in the second incubation week.Soil min-eralization rate and nitrification rate decreased with the increase of stand ages and successive rotations,but the stand ages and successive rotations had no obvious effect on ammonification rate.For all stud-ied sites,the cumulative mineralized N and mineralization rate were significantly greater at the incuba-tion temperature of 30℃ than at the temperature of 20℃ ,indicating that incubation temperature had a great influence on soil mineralization.