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1.
碳酸氢根和铵态氮共同对菜豆生长及养分吸收的影响 总被引:5,自引:1,他引:5
以菜豆为材料进行水培试验, 探讨了高浓度NH4+-N与HCO3-共存介质对菜豆生长发育及其营养吸收的影响, 结果表明: ①以HCO3--N 为主要氮源时, 菜豆生长状况最好; 以NH4+-N为主要氮源且无HCO3-存在时, 培养前期菜豆根系就发生受害现象, 叶片出现萎蔫; 但加入HCO3-后, 随着营养液中HCO3- 浓度从0 升高到13. 0 mmol/L , 菜豆长势逐渐改善, 表明HCO3-与NH4+ 以较合适的比例共存于介质中可明显减轻二者非共存对菜豆生长的抑制作用。② 同一处理, 菜豆整株对主要营养元素吸收量的次序为: N > K> P > Ca >Mg > Fe >Mn , 以NH4+2N 为主要氮源时, 随HCO3-浓度升高, 菜豆对N、P、Ca、Mn 的吸收量逐渐增大。③以NO3--N 为主要氮源, P、Fe、Mn 元素在根部出现累积, 而以NH4+-N为主要氮源时, 随HCO3-浓度增加, N、P、Ca、Mn 在根部亦有累积现象。 相似文献
2.
3.
覆膜滴灌条件下,采用静态箱-气相色谱法研究了不同施肥策略:CK(不施肥)、CF(N 300 kg/hm~2;P2O590 kg/hm~2;K2O 60 kg/hm~2)、60%CF+OF(普通有机肥6 000 kg/hm~2)、60%CF+BF(生物有机肥6 000 kg/hm~2)对棉田土壤N_2O排放的影响,旨在明确滴灌棉田连续不同施肥策略下土壤N_2O的排放特征。结果表明,棉花生育期N_2O排放通量表现为施肥处理大于不施肥处理,滴灌施肥后第3/4天N_2O排放通量顺序为CF60%CF+OF60%CF+BFCK,而滴灌后第7/8天N_2O排放通量则表现为有机肥处理高于化肥处理,滴灌施肥结束后表现与之相同;生育期的N_2O排放总量以100%化肥处理(CF)最高,与其相比,60%CF+OF和60%CF+BF处理分别降低3.75%和8.37%,N_2O排放系数则分别降低1.39%和73.8%;相关及通径分析均表明,与土壤NH+4-N相比,NO-3-N与N_2O排放的关系更密切。 相似文献
4.
氯化铵作为小麦的氮肥施用,营养平衡时,其肥效与硫铵相近;小麦籽粒粗蛋白总量、面筋含量、蛋白质各组分含量亦差异不大。若麦体营养不平衡时,则氯铵肥效降低、吸氯量增加,氯毒害加重,明显影响小麦产量、品质及生长发育,且降低麦株对N.P.K的累积量。施入土壤中的氯化铵,约5-10%的氯为小麦吸收,约5%残留在耕层土壤中,余则在当季作物期间被淋洗。小麦吸收的氯主要分布在叶片和茎杆中,约占95%,很少向穗部运转。 相似文献
5.
套种不同牧草的果园土壤对铵的吸附特性研究 总被引:1,自引:0,他引:1
以套种不同牧草的果园土壤为研究对象,通过室内等温吸附实验,分析比较了各个处理对氨态氮的吸附特性,并将结果用不同的数学模型拟合进行分析.结果表明:当土壤的氨浓度超过一临界值时,其对氨离子的吸附量会出现明显上升,而在此临界值以下则变化不明显;套种不同牧草可不同程度地提高土壤的铵吸附能力,具体表现为圆叶决明>百喜草>平托花生>宽叶雀稗>CK(自然生日本草);各处理土壤铵等温吸附与多项式拟合效果最佳,与Freundlich、Temkin方程拟合达显著水平,Langmuir方程的拟合结果较差. 相似文献
6.
《Communications in Soil Science and Plant Analysis》2012,43(19):2358-2370
The soil phosphorus (P) test in Portugal is based on extraction with ammonium lactate (AL) at acidic pH. Because this test is rarely used in other countries, it is desirable to see whether the AL-P values correlate with the more commonly used P tests. In this work, we compared AL-P with bicarbonate-extractable P (Olsen's method) for a group of 48 samples from Portuguese acidic soils differing widely in P status. Despite their contrasting composition, both reagents extracted phosphate from the same sources, albeit in different proportions. Both Olsen P and AL-P were strongly correlated with resin-extractable and dilute electrolyte-desorbable P, which are respectively related to the soil contents in phytoavailable P and P that can be released to runoff or drainage water. Olsen P and AL-P were strongly correlated (R2 = 0.870), the correlation became stronger when three overfertilized soils were excluded (Olsen P = 2.35 + 0.45 AL-P; R2 = 0.908; P ≤ 0.001, n = 45). No correlation was observed for a group of soils recently fertilized with Gafsa phosphate probably because the acidic AL reagent dissolved residual calcium phosphate, thus overestimating the soil content in desorbable P. On the basis of the present results and the AL-P-based fertility classes used for fertilizer recommendation purposes, Olsen P–based fertility classes were tentatively proposed for Portuguese acidic soils. 相似文献
7.
《Communications in Soil Science and Plant Analysis》2012,43(6):663-672
Abstract A comparison was made of automated procedures and steam distillation for analysis of NH4 + and NO3 ‐ in KCl extracts of soils. Automated analysis of NH4 + utilized the phenate‐hypochlorite reaction. Nitrate was analyzed by E. coli reduction of NO3 ‐ to NO2‐which was then determined colorimetrically by reaction with sulfanilamide and napthylethylenediamine diHCl. Soil extracts were made with 1 M and 2 M KCl. Extracting with 1 M KCl was as effective as 2 M KCl. Extracts in 1 M KCl did not interfere with E. coli reduction of NO3‐, but 2 M KCl did. The automated procedures when compared to distillation gave similar if not better precision and reduced variation particularly at low N concentrations. The automated procedure tended to give higher values at higher NO3‐concentrations. Reduced time required for the analyses provided an additional advantage for the automated procedures. 相似文献
8.
A laboratory study was conducted at the Indian Agricultural Research Institute, New Delhi on a sandy clay loam soil of pH 7.9 and organic C content of 0.34% to study the effect of incorporating Sesbania or Vigna legume residues or wheat straw at 15 and 30t ha?1 on temporal variation in ammoniacal and nitrate‐N in soil under submergence and well drained conditions. Under submergence most mineral N was present as ammoniacal‐N, while under well drained conditions it was present as Nitrate‐N. The content of ammoniacal N in soil was the highest after 30 days of incubation and declined thereafter under submergence. On the other hand under well drained conditions the mineral‐N (mostly nitrate) content in soil at 30 DAI was very little and showed increases only later, reaching the highest level at 90 DAI. Application of wheat straw specially at 301 ha?1 level resulted in immobilization of native soil‐N. These results show that rice which is grown under submergence can be transplanted soon after incorporation of legume residues, but for wheat or other crops which are grown under well drained condition a time interval of 30 days or more needs to be provided before sowing the crop. 相似文献
9.
《Soil biology & biochemistry》2011,43(6):1285-1291
Two common plant species of temperate wet grasslands, Carex acuta and Glyceria maxima, were tested for their preferences in the uptake of different nitrogen (N) sources (amino acid, ammonium, nitrate) and their ability to compete for these sources with soil microorganisms. The experiment was a one-day incubation study with plants growing in soil obtained from the field, which was supplied with a solution containing the three N sources, one at a time labeled with 15N. The bulk of the N demand of both species was covered by nitrate-N, which was the dominant N form in the soil at the time of the experiment. Ammonium-N was taken up less strongly, and organic N formed only a negligible part of their nutrition. The assimilated inorganic N was preferentially transported to apical meristem of the youngest leaf, while organic N remained mostly in the roots. The fast-growing Glyceria took up more N and was a better competitor vis-à-vis soil microbes for rarer N forms than Carex. However, both plants were poor competitors for N vis-à-vis soil microbes, irrespective of the N form. Microbes took up nitrate ca. five times faster and organic N more than a hundred times faster than plants. Correspondingly, the calculated turnover time of microbial N was 17 days, compared to 40 days for N in plant roots. A significant amount of added 15N was found at non-exchangeable sites in the soil, which points to the importance of microbial N transformation and abiotic N fixation for N retention in soil. In summary, the preferential assimilation of inorganic N by the wetland plants studied here and their poor ability to compete for N with soil microbes over the short term agree with the results of studies carried out with other species from temperate grasslands. 相似文献
10.
R. P. Smart L. J. Calver A. M. Crowe K. M. Emmerson & M. S. Cresser 《Soil Use and Management》2007,23(3):317-322
Leaching of inorganic N species to stream waters from upland areas of the UK is increasing, reflecting the increases in atmospheric deposition of nitrogen species due to increased levels of vehicular emissions. Bracken cover in UK uplands is also increasing overall ( Taylor, 1986 ), and the architectural nature of bracken has been shown to both increase deposition of atmospheric constituents to soils and change their chemical and physical nature. We have tested the nutrient status of upland podzols from the Lake District, Cumbria, UK, from under both moorland grass and bracken. The results show reduced levels of base cations and nitrate throughout the profile and decreases in the organic matter content of surface horizons as a consequence of bracken encroachment. We also report increased ammonium concentrations in lower soil horizons under bracken, possibly leading to increased leaching to stream waters. These results suggest either increased leaching of soil nutrients due to bracken encroachment or increased storage of nutrients within the bracken rhizome system. Results also suggest changes in either microbial activity or the microbial community of podzols, possibly due to the allelopathic nature of bracken. This may have caused changes in the soil nutrient dynamics, possibly accounting for some of the changes seen. We hypothesize that increased bracken cover within the British uplands has the potential to increase leaching of inorganic nitrogen to upland streams. 相似文献