福建农业学报
福建農業學報
복건농업학보
FUJIAN JOURNAL OF AGRICULTURAL SCIENCES
2015年
4期
394-399
,共6页
陈玉真%王峰%尤志明%吴志丹%江福英%张文锦%翁伯琦
陳玉真%王峰%尤誌明%吳誌丹%江福英%張文錦%翁伯琦
진옥진%왕봉%우지명%오지단%강복영%장문금%옹백기
茶园土壤%施氮量%氮素淋失
茶園土壤%施氮量%氮素淋失
다완토양%시담량%담소림실
tea garden soil%nitrogen application rate%nitrogen leaching
为研究不同施氮量对茶园土壤氮淋失的影响,改良茶园土壤品质,采用室内土柱淋滤试验,研究不同施氮量对强酸性茶园土壤淋溶液pH、N H+4‐N和NO3-‐N淋溶量的影响。氮肥采用尿素,氮肥用量分别为N0(0 kg · hm -2)、N1(150 kg · hm -2)、N2(300 kg · hm -2)、N3(450 kg · hm -2)、N4(600 kg · hm -2)。结果表明:施用氮肥降低了土壤p H和土壤淋溶液p H ,降低幅度分别为0.08~0.32和0.35~0.81个单位,促进茶园土壤酸化;N H+4‐N和N O3-‐N的淋溶量均随施氮量的增加而提高;无机氮的淋失率为47.66%~71.31%,淋失量(Y)与施氮量(X)之间的线性回归方程为Y=0.708X+145.27(R2=0.98);在整个淋洗过程中,NH+4‐N和NO3-‐N淋溶主要发生在前5次,且主要以NO3-‐N的形式淋失,淋失比例为73.50%~89.21%。
為研究不同施氮量對茶園土壤氮淋失的影響,改良茶園土壤品質,採用室內土柱淋濾試驗,研究不同施氮量對彊痠性茶園土壤淋溶液pH、N H+4‐N和NO3-‐N淋溶量的影響。氮肥採用尿素,氮肥用量分彆為N0(0 kg · hm -2)、N1(150 kg · hm -2)、N2(300 kg · hm -2)、N3(450 kg · hm -2)、N4(600 kg · hm -2)。結果錶明:施用氮肥降低瞭土壤p H和土壤淋溶液p H ,降低幅度分彆為0.08~0.32和0.35~0.81箇單位,促進茶園土壤痠化;N H+4‐N和N O3-‐N的淋溶量均隨施氮量的增加而提高;無機氮的淋失率為47.66%~71.31%,淋失量(Y)與施氮量(X)之間的線性迴歸方程為Y=0.708X+145.27(R2=0.98);在整箇淋洗過程中,NH+4‐N和NO3-‐N淋溶主要髮生在前5次,且主要以NO3-‐N的形式淋失,淋失比例為73.50%~89.21%。
위연구불동시담량대다완토양담림실적영향,개량다완토양품질,채용실내토주림려시험,연구불동시담량대강산성다완토양림용액pH、N H+4‐N화NO3-‐N림용량적영향。담비채용뇨소,담비용량분별위N0(0 kg · hm -2)、N1(150 kg · hm -2)、N2(300 kg · hm -2)、N3(450 kg · hm -2)、N4(600 kg · hm -2)。결과표명:시용담비강저료토양p H화토양림용액p H ,강저폭도분별위0.08~0.32화0.35~0.81개단위,촉진다완토양산화;N H+4‐N화N O3-‐N적림용량균수시담량적증가이제고;무궤담적림실솔위47.66%~71.31%,림실량(Y)여시담량(X)지간적선성회귀방정위Y=0.708X+145.27(R2=0.98);재정개림세과정중,NH+4‐N화NO3-‐N림용주요발생재전5차,차주요이NO3-‐N적형식림실,림실비례위73.50%~89.21%。
To improve strongly‐acidified soil quality of tea garden ,a laboratory simulation test of column‐leach was carried out to investigate the effects of applying different nitrogen rates on the pH ,ammonium nitrogen (NH+4 ‐N) and nitrate nitrogen (NO3-‐N ) of soil leachate .With urea as nitrogen fertilizer , the different applications were respectively treated with N0 (0 kg · hm -2 ) ,N1 (150 kg · hm -2 ) ,N2 (300 kg · hm-2 ) ,N3 (450 kg · hm-2 ) and N4 (600 kg · km -2 ) .The results showed that the pH values of soil leachate were be decreased by 0.08~0.32 and 0.35~0.81 with different N application rates ,resulting in more soil acidification .The leaching amounts of NH+4 ‐N and NO3-‐N were increased by increasing rates of nitrogen fertilizer ,and 47.66% ~71.31% inorganic nitrogen was lost in leaching water .The regression equation between inorganic nitrogen loss (Y ) and N application rates (X) was Y = 0.708 X + 145.27 (R2 =0.98) .The leaching of NH+4 ‐N and NO3-‐N majorly occurred at the first five times , and the leaching amounts of NO3-‐N accounted for 73.50% ~89.21% of the total leaching inorganic nitrogen .