农业工程学报
農業工程學報
농업공정학보
2014年
6期
54-61
,共8页
高德才%张蕾%刘强%荣湘民%张玉平%田昌
高德纔%張蕾%劉彊%榮湘民%張玉平%田昌
고덕재%장뢰%류강%영상민%장옥평%전창
氮%土壤%碳%生物炭%淋洗%硝态氮%铵态氮
氮%土壤%碳%生物炭%淋洗%硝態氮%銨態氮
담%토양%탄%생물탄%림세%초태담%안태담
nitrogen%soils%carbon%biochar%leaching%nitrate nitrogen%ammonium nitrogen
该试验采用土柱室内模拟的方法,旱地土壤上分别添加不同比例的生物炭(0、0.5%、2%、4%、6%、8%),通过模拟降雨淋洗,探讨生物炭对旱地土壤氮素动态变化的影响。结果表明:添加生物炭能延缓 NO3-和总氮淋洗速度,生物炭添加质量百分数达2%及以上时,可显著降低总氮和 NH4+淋洗,其添加质量百分数达4%及以上时,可显著降低NO3-淋洗,而添加少量生物炭对氮的淋洗无影响;NO3-淋洗量占旱地土壤氮素淋洗总量的84%~90%,而NH4+仅占0.4%~2%;各处理下不同土层间土壤全氮含量均无差异,而不同处理间土壤全氮含量差异显著,当生物炭添加质量百分数达2%及以上时,土壤全氮含量随生物炭添加量的增加而增加,且生物炭添加百分数与土壤全氮之间满足极显著的指数关系(R2=0.9944)。因此,在旱地土壤上施用生物炭量至少达2%以上才能显著减少氮素淋洗和增加土壤全氮含量,达到减少土壤氮素损失和提高氮素利用率,减少由氮素带来的环境污染以及改善土壤肥力的综合目标。
該試驗採用土柱室內模擬的方法,旱地土壤上分彆添加不同比例的生物炭(0、0.5%、2%、4%、6%、8%),通過模擬降雨淋洗,探討生物炭對旱地土壤氮素動態變化的影響。結果錶明:添加生物炭能延緩 NO3-和總氮淋洗速度,生物炭添加質量百分數達2%及以上時,可顯著降低總氮和 NH4+淋洗,其添加質量百分數達4%及以上時,可顯著降低NO3-淋洗,而添加少量生物炭對氮的淋洗無影響;NO3-淋洗量佔旱地土壤氮素淋洗總量的84%~90%,而NH4+僅佔0.4%~2%;各處理下不同土層間土壤全氮含量均無差異,而不同處理間土壤全氮含量差異顯著,噹生物炭添加質量百分數達2%及以上時,土壤全氮含量隨生物炭添加量的增加而增加,且生物炭添加百分數與土壤全氮之間滿足極顯著的指數關繫(R2=0.9944)。因此,在旱地土壤上施用生物炭量至少達2%以上纔能顯著減少氮素淋洗和增加土壤全氮含量,達到減少土壤氮素損失和提高氮素利用率,減少由氮素帶來的環境汙染以及改善土壤肥力的綜閤目標。
해시험채용토주실내모의적방법,한지토양상분별첨가불동비례적생물탄(0、0.5%、2%、4%、6%、8%),통과모의강우림세,탐토생물탄대한지토양담소동태변화적영향。결과표명:첨가생물탄능연완 NO3-화총담림세속도,생물탄첨가질량백분수체2%급이상시,가현저강저총담화 NH4+림세,기첨가질량백분수체4%급이상시,가현저강저NO3-림세,이첨가소량생물탄대담적림세무영향;NO3-림세량점한지토양담소림세총량적84%~90%,이NH4+부점0.4%~2%;각처리하불동토층간토양전담함량균무차이,이불동처리간토양전담함량차이현저,당생물탄첨가질량백분수체2%급이상시,토양전담함량수생물탄첨가량적증가이증가,차생물탄첨가백분수여토양전담지간만족겁현저적지수관계(R2=0.9944)。인차,재한지토양상시용생물탄량지소체2%이상재능현저감소담소림세화증가토양전담함량,체도감소토양담소손실화제고담소이용솔,감소유담소대래적배경오염이급개선토양비력적종합목표。
Excessive application of nitrogen fertilizer in agricultural soils is considered as a main cause of ecological problems such as nitrogen leaching, which has become an important limitation to improving nitrogen use efficiency in agricultural production. Because of its physical, chemical, and biological stability, biochar when applied to soils can play a key role in nutrient cycling, potentially affecting nitrogen retention and improving soil fertility. However, experimental results were variable and dependent on the experimental set-up, soil properties, and fertilizer application rates and biochar were set up at the high and low levels, which possess a big blind area. A laboratory experiment was conducted to investigate the effects of biochar additions on dynamic changes of nitrogen under artificial rainfall conditions by adding 0, 0.5%, 2%, 4%, 6%, and 8% biochar (the biochar was prepared by pyrolyzing corn straw at 500-550℃ under oxygen limited condition) into soil columns collected from red dryland of southern China under urea application condition (300 kg/hm2). The results showed that the speed of leaching of NO3-and total nitrogen was delayed by biochar applications. Compared with urea application treatment, the total nitrogen and NH4+ contents in leachate were significantly decreased by 4.02% and 8.93%when ≥2% biochar was applied into soil, and the NO3- contents of leachate was obviously decreased by 3.23%-11.87%when the biochar ratio reached 4%. But there was no significant effect of adding small amount of biochar (such as 0.5%) on N leaching compared with urea application treatment. Leaching losses of NO3- had been found to be highest because the NO3-was mobile, and may not be taken up by plants. NO3-leaching amount accounted for 84%-90%of the total nitrogen leaching amount, while NH4+leaching only accounted for 0.4%-2%;The total nitrogen content of different soil layers in each treatment was similar regardless of the fertilization and biochar applications. While the total nitrogen contents in soils were markedly different among the treatments. Compared with urea application treatment, the content of soil total nitrogen was significantly increased by 4.62%to 10.62%when biochar addition was≥2%, and the relationship between addition amounts of biochar (x) and the content of soil total nitrogen (y) followed an index equation: y=1.6e0.0845x (R2=0.99, n=24). The results above suggested that biochar could be used as a potential additive for nutrient retention in order to increase the utilization efficiency of chemical fertilizers. In conclusion, biochar additions could decrease the leaching amount of NH4+, NO3-and total nitrogen and partly increased the concentration of soil total nitrogen. However, the low biochar addition had no significant effects on reducing nitrogen leaching and increasing soil total nitrogen content. Therefore, the purpose to obviously decrease nitrogen leaching and increase the content of soil total nitrogen could be realized only when biochar addition was above 2% in dryland soil. Nonetheless, the effect of biochar addition on reducing soil nitrogen leaching needs to be further verified before biochar can be applied to agricultural fields on a large scale.