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Symbiotic N2 fixation by soybean in organic and conventional cropping systems estimated by 15N dilution and 15N natural abundance

机译:通过15 N稀释和15 N自然丰度估算有机和常规种植系统中大豆对共生N2 的固定

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Nitrogen (N) is often the most limiting nutrient in organic cropping systems. N2 fixing crops present an important option to improve N supply and to maintain soil fertility. In a field experiment, we investigated whether the lower N fertilization level and higher soil microbial activity in organic than conventional systems affected symbiotic N2 fixation by soybean (Glycine max, var. Maple Arrow) growing in 2004 in plots that were since 1978 under the following systems: bio-dynamic (DYN); bio-organic (ORG); conventional with organic and mineral fertilizers (CON); CON with exclusively mineral fertilizers (MIN); non-fertilized control (NON). We estimated the percentage of legume N derived from the atmosphere (%Ndfa) by the natural abundance (NA) method. For ORG and MIN we additionally applied the enriched 15N isotope dilution method (ID) based on residual mineral and organic 15N labeled fertilizers that were applied in 2003 in microplots installed in ORG and MIN plots. These different enrichment treatments resulted in equal %Ndfa values. The %Ndfa obtained by NA for ORG and MIN was confirmed by the ID method, with similar variation. However, as plant growth was restricted by the microplot frames the NA technique provided more accurate estimates of the quantities of symbiotically fixed N2 (Nfix). At maturity of soybean the %Ndfa ranged from 24 to 54%. It decreased in the order ORG > CON > DYN > NON > MIN, with significantly lowest value for MIN. Corresponding Nfix in above ground plant material ranged from 15 to 26 g N m-2, with a decreasing trend in the order DYN = ORG > CON > MIN > NON. For all treatments, the N withdrawal by harvested grains was greater than Nfix. This shows that at the low to medium %Ndfa, soybeans did not improve the N supply to any system but removed significant amounts of soil N. High-soil N mineralization and/or low-soil P availability may have limited symbiotic N2 fixation.
机译:氮(N)通常是有机耕作系统中最限制性的养分。固氮作物是提高氮素供应和维持土壤肥力的重要选择。在田间试验中,我们调查了在2004年开始种植的田间,较低的氮肥水平和较高的土壤微生物活性是否会比常规系统中的大豆对大豆(Glycine max,var。Maple Arrow)种植的共生固氮菌产生影响。 1978年采用以下系统:生物动力(DYN);生物有机(ORG);常规使用有机和矿物肥料(CON);与纯矿物肥料(MIN)混用;非受精对照(NON)。我们通过自然丰度(NA)方法估算了来自大气的豆类N的百分比(%Ndfa)。对于ORG和MIN,我们还基于残留的矿物和有机15 N标记的肥料,另外应用了富集的15 N同位素稀释法(ID),该肥料于2003年在ORG和MIN样地中安装的微坑中使用。这些不同的浓缩处理导致%Ndfa值相等。通过ID法确定了NA对ORG和MIN所获得的%Ndfa,具有相似的变化。但是,由于植物的生长受到微图框架的限制,因此NA技术可以更准确地估计共生固定的N2 (Nfix)的数量。大豆成熟时,Ndfa的百分比为24%至54%。它以ORG> CON> DYN> NON> MIN的顺序降低,MIN的值最低。地上植物材料中相应的Nfix范围为15至26 g N m-2 ,其下降趋势为DYN = ORG> CON> MIN> NON。对于所有处理,收获谷物的氮素吸收量均大于Nfix。这表明在低至中等含量的Ndfa时,大豆不能改善任何系统的氮供应,但会去除大量的土壤N。高土壤氮矿化和/或低土壤磷的有效利用可能会限制共生N2 固定。

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