首页> 外文期刊>Geoderma: An International Journal of Soil Science >The effects of N and P additions on microbial N transformations and biomass on saline-alkaline grassland of Loess Plateau of Northern China.
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The effects of N and P additions on microbial N transformations and biomass on saline-alkaline grassland of Loess Plateau of Northern China.

机译:N和P添加对北方黄土高原盐碱草原微生物N转化和生物质的影响。

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Microbial nutrient transformation plays an important role in regulating nitrogen (N) and phosphorus (P) cycling in terrestrial ecosystems. Soil N and P contents also control microbial nutrient transformations. However, there is still dispute on how N and P additions affect microbial activity and N transformations. A field experiment was conducted to examine the effects of N and P on microbial N transformations and biomass in saline-alkaline grassland in Loess Plateau of northern China during growing season in 2009. N was added at a rate of 10 g N m-2 y-1 in the form of NH4NO3. P was added at a rate of 5 g P m-2 y-1 in the form of P2O5-. We measured the in situ net ammonification rate (Ramm), and nitrification rate (Rnit) once a month from May to October; we also measured potential soil microbial biomass carbon (MBC), nitrogen (MBN), and potential microbial respiration (MR) once a month in laboratory. Results: During the whole growing seasons, P addition significantly stimulated soil inorganic N pool, soil extractable C, soil extractable N pool, Rmin, and the metabolic quotient (qCO2) from the estimates of microbial respiration and microbial biomass carbon, and there was no effect on peak aboveground biomass, MBC, MBN and MR during the whole growing seasons in 2009. N addition significantly increased peak aboveground biomass, inorganic N pool, Rmin, MBN, MR, and qCO2, decreased soil extractable C and the ratio of MBC/MBN, and there was no effect on soil extractable N and MBC during the growing season in 2009. P addition increased the soil net N mineralization rate and N addition not only increased the soil net N mineralization rate but also increased microbial biomass N. We observed that P induced a decreased soil inorganic N pool, but N addition directly increased soil inorganic N pool, how to balance the quantity of N and P additions in agriculture system is an important technique in agriculture harvest in the future in Loess Plateau of Northern China.
机译:微生物营养转化在调节氮气(n)和循环陆生态系统中的循环中起着重要作用。土壤N和P含量也控制微生物营养转化。然而,仍然有关N和PACTION如何影响微生物活动和N变换的争议。进行了田间实验,以检查2009年生长季节在中国北方黄土高原盐水 - 碱性草原上对微生物N转化和生物质的影响。n以10g n m 的速率加入-2 y -1 -1 以nh 4 no 3 。 P 2 O 5的形式以5g p m -2 -2 -2 -2 y -1 / sup>的速率加入p。 sub> - 。我们测量原位净氨化率(R AMM ),并从5月到10月份每月一次硝化率(R NIT );我们还测量了潜在的土壤微生物碳(MBC),氮气(MBN)和潜在的微生物呼吸(MR)在实验室中每月一次。结果:在整个生长季节期间,P添加显着刺激土壤无机N池,土壤可萃取物C,土壤萃取物N池,R <亚>分钟,以及代谢商(QCO 2 )从微生物呼吸和微生物生物量碳的估计,2009年整个生长季节的地上生物量>分钟,MBN,MR和QCO 2 ,降低土壤可提取物C和MBC / MBN的比例,并且在生长季节期间对土壤可提取的N和MBC没有影响2009. P添加增加土壤净矿化率和N添加不仅增加了土壤净矿化率,而且还增加了微生物生物量增加了。我们观察到P诱导土壤无机N池的降低,但是N添加的土壤无机N.池,如何平衡N和P添加的数量农业制度是中国北方黄土高原未来农业收获的重要技术。

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