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81.
有机肥与无机肥配施对菜地土壤N2O排放及其来源的影响 总被引:1,自引:1,他引:0
该研究采用同位素自然丰度法,通过室内培养试验研究北京地区菜地有机肥和无机肥配施对土壤释放N2O及同位素位嗜值SP(site preference)的影响,以期获得不同肥料及其配比下土壤N2O的来源及变化规律。结果表明:施用无机肥释放的N2O显著高于有机肥,其累积排放量是有机肥的6.63倍,且无机肥施用比例越高,排放量越大;各肥料组合在施用后7天内均以反硝化作用生成N2O为主,贡献最高达到78.89%,SP为6.97‰,之后硝化作用逐渐增强并成为主要途径,最高占比达76.48%,SP为25.24‰;培养期内施用无机肥可以促进反硝化作用,平均占比52.98%,SP为15.52‰,而有机肥会使硝化作用增强,平均占比71.35%,SP为23.55‰。因此,在北京潮褐土地区菜地土壤施用有机肥对N2O有良好的减排效果,可为蔬菜生产中肥料的合理应用提供科学依据。 相似文献
82.
本研究优化了采用反硝化细菌法同时测定土壤浸提液中硝酸盐氮氧同位素组成的方法。在已有研究结果的基础上,通过采用5000~8000 r·min-1的转速离心、高纯氮气吹扫1 h、减少加样量及改造仪器自动进样器等措施对已发表方法进行了优化。对国际标准样品USGS34的分析表明,0.1~0.8μg NO-3-N样品量即可以得到较稳定、准确的测定值和校正值;同一时间内制备的硝酸盐δ15N的SD介于0.05‰~0.09‰之间,δ18O的SD介于0.28‰~0.48‰之间;在三个月之内δ15N和δ18O的测定值基本一致,表明该方法具有较好的准确度、精密度和稳定性。通过研究浸提剂、保存条件以及加热对测定土壤浸提液中硝酸盐氮氧同位素组成的影响,结果表明:常用的去离子水、KCl、Ca Cl2可能都含有微量的硝酸盐,随着加样量增大,浸提剂中含有的硝酸盐可能就会影响δ15N和δ18O的测定;对于土壤硝酸盐的浸提液,冷冻保存效果较好,保证了土壤硝酸盐氮氧同位素的准确性和稳定性;尽管加热对硝酸盐标准样品USGS34和IAEA-NO3的δ15N没有显著影响,但δ18O显著升高,说明加热易引起氧同位素分馏;而土壤硝酸盐浸提液样品加热前后的δ15N和δ18O的测定值没有显著变化,因此为避免产生氧同位素分馏和节省测试时间,建议同时测定土壤浸提液硝酸盐δ15N和δ18O时直接和反硝化细菌反应。应用本方法对不同肥料处理田间土壤浸提液硝酸盐的氮氧同位素组成进行了测定。 相似文献
83.
84.
为进一步掌握江苏近海金乌贼(Sepia esculenta)种群生活史特征,根据在江苏沿海港口所采集的样本,利用碳氮稳定同位素分析法对金乌贼的摄食生态及营养生态位进行了研究。结果表明,金乌贼雌、雄群体间 13C和 15N值均不存在显著性差异;金乌贼的 值与胴长之间相关性不显著, 值与胴长之间存在显著相关性;雄性金乌贼营养生态位宽度(SEAc=0.57‰2)与雌性(SEAc=0.63‰2)无明显差异,雌性略大于雄性,且两者高度重叠(0.62)。同位素聚类分析显示,可将金乌贼个体分为75~114mm、115~184mm和185~204mm三个胴长组;185~204mm胴长组营养生态位宽度最大(SEAc=1.77‰2),75~114mm胴长组营养生态位宽度最小(SEAc=0.39‰2);仅75~114mm和115~184mm胴长组间生态位重叠率为中度重叠(0.34),其余胴长组间生态位重叠率低。分析认为,金乌贼δ13C值的变化主要受同位素基线值和金乌贼洄游模式影响,而δ15N值的变化主要受金乌贼摄食作用影响;雌性和雄性金乌贼群体之间食物资源和栖息地利用高度相似;不同发育阶段的金乌贼在营养生态位上具有明显差异。 相似文献
85.
Relationship between stable carbon isotope discrimination and water use efficiency under regulated deficit irrigation of pear-jujube tree 总被引:2,自引:0,他引:2
Ningbo Cui Taisheng Du Shaozhong Kang Fusheng Li Xiaotao Hu Mixia Wang Zhijun Li 《Agricultural Water Management》2009,96(11):1615-1622
To investigate the relationship between stable carbon isotope discrimination (Δ) of different organs and water use efficiency (WUE) under different water deficit levels, severe, moderate and low water deficit levels were treated at bud burst to leafing, flowering to fruit set, fruit growth and fruit maturation stages of field grown pear-jujube tree, and leaf stable carbon isotope discrimination (ΔL) at different growth stages and fruit stable carbon isotope discrimination (ΔF) at fruit maturation stage were measured. The results indicated that water deficit had significant effect on ΔL at different growth stages and ΔF at fruit maturation stage. As compared with full irrigation, the average ΔL at different growth stages and ΔF at fruit maturation stage were decreased by 1.23% and 2.67% for different water deficit levels, respectively. ΔL and ΔF among different water deficit treatments had significant difference at the same growth stage (P < 0.05). Under different water deficit conditions, significant relationships between the ΔL and WUEi (photosynthesis rate/transpiration rate, Pn/Tr), WUEn (photosynthesis rate/stomatal conductance of CO2, Pn/gs), WUEy (yield/crop water consumption, Y/ETc) and yield, or between the ΔF and WUEy and yield were found, respectively. There were significantly negative correlations of ΔL with WUEi, WUEn, WUEy and yield (P < 0.01) at the fruit maturation stage, or ΔL with WUEi and WUEn (P < 0.01) over whole growth stage, respectively. ΔF was negatively correlated with WUEy, WUEn and yield (P < 0.05), but positively correlated with ETc (P < 0.01) over the whole growth stage. Thus ΔL or ΔF can compare WUEn and WUEy, so the stable carbon isotope discrimination method can be applied to evaluate the water use efficiency of pear-jujube tree under the regulated deficit irrigation. 相似文献
86.
87.
Twenty cowpea (Vigna unguiculata L. Walp.) genotypes, comprising Kenyan cultivars and Kenyan and introduced breedings lines, were grown in 15 replicated field trials carried out at three locations in semi-arid eastern Kenya over four seasons. Grain and straw yields and the carbon isotope discrimination (Δ) of this material were determined, and days to flowering and maturity observed.None of the seasons in which the trials were conducted was appreciably drier than the long term average for the sites, and some trials received excessive rain. Averaging the data for the 15 trials, one genotype yielded much less grain (77 g m−2) than the 19 others, whose yield ranged from 125 to 177 g m−2 (average 148 g m−2). Trial mean yield trials had a high straw Δ (r = +0.567) and had received more rain between flowering and maturity (r = +0.428) than lower yielding ones. Among genotypes, averaging over trials, the correlation coefficient (r) between grain yield and grain Δ was +0.394, and between grain yield and straw Δ, +0.460. Early genotypes had the highest grain Δ and straw Δ. The correlation among genotypes between date of flowering and grain Δ was −0.632 and with straw Δ, −0.502. When comparisons were made among trials, there was no clear relationship between the strength of the correlations among genotypes between grain yield and straw Δ or grain Δ and the degree of stress experienced by a trial (as indicated by the rainfall it had received). It appeared that this was because the variances of grain Δ and straw Δ were greater in the most droughted trials, whereas the variance of yield was greatest in the least droughted trials.It is concluded that the genetic correlation between grain yield and either grain Δ or straw Δ is unlikely to be strong enough to make either Δ a useful surrogate or adjunct in selecting for high yield in the segregating generations of a breeding programme for semi-arid eastern Kenya, but that Δ may be of value in the selection of parent genotypes. 相似文献
88.
89.
The present study focuses on the microbial recalcitrance of pyrogenic organic material (PyOM) on a molecular scale. We performed microcosm incubation experiments using 13C- and 15N-enriched grass-derived PyOM mixed with a sub soil material taken from a Haplic Cambisol. Solid-state 13C and 15N NMR studies were conducted to elucidate the humification processes at different stages of PyOM degradation. The chemical structure of the remaining PyOM after incubation was clearly different from the initial pyrogenic material. The proportion of O-containing functional groups was increased, whereas that of aryl C and of N-containing heterocyclic structures had decreased, probably due to mineralisation and conversion to other C and N groups. After 20 months of incubation the aryl C loss reached up to 40% of the initial amount and up to 29% of the remaining PyOM C was assigned to carboxyl/carbonyl C and O-aryl C. These reactions alter the chemical and physical properties of the char residue and make it more available for further microbial attack but also for adsorption processes. Our study presents direct evidence for the degradation of N-heterocyclic domains in charred plant remains adding new aspects to the understanding of the N cycling in fire-affected ecosystems. 相似文献
90.