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71.
Increased root exudation and a related stimulation of rhizosphere-microbial growth have been hypothesised as possible explanations for a lower nitrogen- (N-) nutritional status of plants grown under elevated atmospheric CO2 concentrations, due to enhanced plant-microbial N competition in the rhizosphere. Leguminous plants may be able to counterbalance the enhanced N requirement by increased symbiotic N2 fixation. Only limited information is available about the factors determining the stimulation of symbiotic N2 fixation in response to elevated CO2.In this study, short-term effects of elevated CO2 on quality and quantity of root exudation, and on carbon supply to the nodules were assessed in Phaseolus vulgaris, grown in soil culture with limited (30 mg N kg−1 soil) and sufficient N supply (200 mg N kg−1 soil), at ambient (400 μmol mol−1) and elevated (800 μmol mol−1) atmospheric CO2 concentrations.Elevated CO2 reduced N tissue concentrations in both N treatments, accelerated the expression of N deficiency symptoms in the N-limited variant, but did not affect plant biomass production. 14CO2 pulse-chase labelling revealed no indication for a general increase in root exudation with subsequent stimulation of rhizosphere microbial growth, resulting in increased N-competition in the rhizosphere at elevated CO2. However, a CO2-induced stimulation in root exudation of sugars and malate as a chemo-attractant for rhizobia was detected in 0.5-1.5 cm apical root zones as potential infection sites. Particularly in nodules, elevated CO2 increased the accumulation of malate as a major carbon source for the microsymbiont and of malonate with essential functions for nodule development. Nodule number, biomass and the proportion of leghaemoglobin-producing nodules were also enhanced. The release of nod-gene-inducing flavonoids (genistein, daidzein and coumestrol) was stimulated under elevated CO2, independent of the N supply, and was already detectable at early stages of seedling development at 6 days after sowing. 相似文献
72.
选择贵州省三种典型的植烟土壤———中性紫色土、黄壤和黄色石灰土为对象,研究了烤烟根际微生物群落结构及其动态变化。结果表明,在烤烟生长过程中,根际细菌的数量在团棵期最低,然后逐渐增加,现蕾期达到峰值,进而又逐渐减少;放线菌和真菌数量从团棵期到成熟期呈增长趋势。土壤类型不同,根际细菌和放线菌的数量不一样,黄壤>黄色石灰土>中性紫色土;真菌数量,中性紫色土>黄壤>黄色石灰土。烤烟根际微生物的种群多样性及其变化在不同土壤中表现也不一样,相对于黄壤和黄色石灰土,在中性紫色土中,根际微生物的优势种群数目较多,根际细菌和放线菌种群更具多样性,而且较稳定,表明其群落结构更为合理,这可能与中性紫色土上的烟草青枯病发生率较低有一定关系。 相似文献
73.
Lisa Bjørnlund Søren Mørk Mette Vestergård Regin Rønn 《Biology and Fertility of Soils》2006,43(1):1-11
The aim was to study the effects of P fertilization and leaf aphid attack on the trophic interactions of bacteria and bacterial feeders in the rhizospheres of barley plants. The density of protozoa peaked in the rhizospheres of plants fertilized with N and P, whereas nematodes peaked in the rhizospheres of plants to which only N had been added. Fingerprinting of bacterial communities by length heterogeneity polymerase chain reaction revealed differences in community structure between NP rhizospheres and N rhizospheres as well as aphid-related differences within N rhizospheres. Specifically, α-proteobacteria increased with P addition. To evaluate if differences in bacteria in terms of their quality as food could partly explain the observed differences in protozoan and nematode abundances, growth of the flagellate Cercomonas sp. was assessed with 935 bacteria isolated from the different treatments. This assay indicated that bacterial isolates were of higher food quality to Cercomonas sp. in NP than in N rhizospheres when plants were subjected to aphid attack. Bacteria of high and low food quality for Cercomonas sp., respectively, were fed to the nematode Caenorhabditis elegans and larval production examined. α-Proteobacteria supported the growth of Cercomonas sp. well, whereas Actinobacteria did not. In contrast, C. elegans reproduced poorly on most α-proteobacteria but were able to reproduce well on some Actinobacteria. These results suggest that the different response of protozoa and nematodes to P addition could be mediated through a food quality-related change in community composition of bacteria and that leaf aphid attack may interfere with nutrient effects on bacterial assemblages of rhizospheres. 相似文献
74.
Rice fields are an important source for atmospheric CH4, but the effects of fertilization are not well known. We studied the turnover of CH4 in rice soil microcosms without and with addition of potassium phosphate. Height and tiller number of rice plants were higher in the fertilized than in the unfertilized microcosms. Emission rates of CH4 were also higher, but porewater concentrations of CH4 were lower. The δ13C values of the emitted CH4 and of the CH4 in the porewater were both 2-6% higher in the fertilized microcosms than in the control. Potassium phosphate did not affect rate and isotopic signature of CH4 production in anoxic soil slurries. On the other hand, roots retrieved from fertilized microcosms at the end of incubation exhibited slightly higher CH4 production rates and slightly higher CH4-δ13C values compared to roots from unfertilized plants. Addition of potassium phosphate to excised rice roots generally inhibited CH4 production and resulted in increasingly lower δ13C values of the produced CH4. Fractionation of 13C during plant ventilation (i.e. δ13C in pore water CH4 versus CH4 emitted) was larger in the fertilized microcosms than in the control. Besides plant ventilation, this difference may also have been caused by CH4 oxidation in the rhizosphere. However, calculation from the isotopic data showed that less than 27% of the produced CH4 was oxidized. Collectively, our results indicate that potassium phosphate fertilization stimulated CH4 emission by enhancing root methanogenesis, plant ventilation and/or CH4 oxidation, resulting in residence times of CH4 in the porewater in the order of hours. 相似文献
75.
J. F. Dormaar 《Biology and Fertility of Soils》1990,10(2):121-126
Summary The effect of one form of soil organic matter, such as living roots or root exudates on another form of soil organic matter, such as dead roots or incorporated litter and litter leachates, has been studied from various perspectives over the last 25 years. The effect seems to be either positive (priming) or negative (conserving). The present review concentrates on the conserving effect, measured as a decrease in 14CO2 released, in both field and greenhouse/growth chamber studies. The field experiments suggested that certain physical conditions in the soil, such as less available moisture or restricted aeration which led to lower microbial activity, explained the conserving effect of living roots on soil organic matter. Although more detailed greenhouse/growth chamber studies confirmed the conserving effect per se, it appears that biological rather than physical factors could better explain the reduction in the rate of decomposition of 14C-labelled plant residues in the presence of roots. However, a complex picture has emerged through a variety of postulates, all proposed in attempts to explain the conserving effect. Finally, the most recent studies have argued that the decrease in decomposition of labelled organic matter in planted soil is probably more apparent than real. A decrease in respired 14CO2 could be explained by an incorporation of 14C derived from old roots into the rhizosphere microbial populations of the living roots. To make any further progress on the fundamental question of how soil organic matter moves along its continuum from a living to a refractory state, the microenvironment needs to be examined at periodic intervals. New developments in improved histochemical and electron-probe microanalyses look promising.LRS Contribution no. 3878970 相似文献
76.
Chantal Hamel Yolande Dalpé Claude Lapierre Régis R. Simard Donald L. Smith 《Biology and Fertility of Soils》1996,21(3):160-165
The dynamics of mycorrhizae under disturbance created by crop production is not well understood. A 3-year experiment was undertaken on a nutrient-poor and acidic land that had last been cultivated in the early 1970s. We observed the effects of cropping spring barley (Hordeum vulgare L.) under four P-fertilizer levels and four levels of lime, in a minimum (rototillage), a reduced (chisel), or a conventional tillage system, on the mycorrhizal receptiveness of the host (maximum level of mycorrhizal colonization, as measured at harvest) and soil infectivity most probable number method. The host receptiveness decreased with time, while crop yields and soil infectivity increased simultaneously with time. Liming increased mycorrhizal colonization of barley roots and soil infectivity. P additions decreased root colonization but did not significantly affect the most probable number valuse. Slightly higher soil infectivity estimates were found under reduced tillage. 相似文献
77.
水稻根际中铁的形态转化 总被引:16,自引:0,他引:16
本文以熟化红壤性水稻土、淀浆白土、红壤和赤红壤为样品,研究了植稻后根际中铁的形态转化.结果表明,两种水稻土根际中无定形氧化铁、游离氧化铁、络合态铁、土壤中氧化铁的活化度及两种红壤上根际中的络合态铁均低于非根际土;而两种红壤上其余各项在根际内外分布趋势均与水稻土相反.用穆斯堡尔谱仪分析表明,所有根际土与非根际土相比,四极矩分裂增大,内磁场下降,说明根际中氧化铁被活化.同时,水稻土上根际中Fe2+增多,赤红壤中根际出现新矿物磁赤铁矿.根际中铁被活化,可能会影响根际中重金属等污染物的吸附和解吸特性、植物的铁素营养及对其它养分的吸收. 相似文献
78.
Growth,P uptake and rhizosphere properties of wheat and canola genotypes in an alkaline soil with low P availability 总被引:1,自引:0,他引:1
Zakaria Solaiman Petra Marschner Dongmei Wang Zed Rengel 《Biology and Fertility of Soils》2007,44(1):143-153
The aim of the present study was to assess the role of soil type on growth, P uptake and rhizosphere properties of wheat and
canola genotypes in an alkaline soil with low P availability. Two wheat (Goldmark and Janz) and two canola genotypes (Drum
and Outback) were grown in a calcareous soil (pH 8.5) at two P levels [no P addition (0P) or addition of 200 mg kg−1 P as Ca3(PO4)2 (200P)] and harvested at flowering or maturity. Shoot and root dry weight, root length and shoot P content were greater in
the two canola genotypes than in wheat. There were no consistent differences in available P, microbial P and phosphatase activity
in the rhizosphere of the different genotypes. Shoot P content was significantly positively correlated with root length, pH
and phosphatase activity in the rhizosphere. The microbial community composition, assessed by fatty acid methylester analysis,
of the canola genotypes differed strongly from that of the wheat genotypes. The weight percentage bacterial fatty acids, the
bacteria/fungi (b/f) ratio and the diversity of fatty acids were greater in the rhizosphere of the canolas than in the rhizosphere of the wheat
genotypes. In contrast to the earlier studies in an acidic soil, only small differences in growth and P uptake between the
genotypes of one crop were detected in the alkaline soil used here. The results confirmed the importance of root length for
P uptake in soils with low P availability and suggest that the rhizosphere microbial community composition may play a role
in the better growth of the canola compared to the wheat genotypes. 相似文献
79.
三七根际链霉菌Streptomyces sp. YNUCC0233木聚糖酶性质研究 总被引:2,自引:0,他引:2
从三七根际分离到一株产木聚糖酶链霉菌Streptomycessp.YNUCC0233。该菌所产生的木聚糖酶的最适反应温度为67℃,最适pH为6.0,在pH5.0~9.0和60℃以下时相对稳定。Ba2+和K+对该木聚糖酶有较强的促进作用,Hg2+、Cu2+、Mn2+、Co2+、Ni2+和EDTA对该酶有较强的抑制作用。对Streptomycessp.YNUCC023316SrDNA的1105bp片段的序列分析结果表明,Streptomycessp.YNUCC0233的16SrDNA片段与GenBank中所有已注册的链霉菌分类单位均不同。 相似文献
80.
Y. N. Song P. Marschner L. Li X. G. Bao J. H. Sun F. S. Zhang 《Biology and Fertility of Soils》2007,44(2):307-314
Cereal/cereal and cereal/legume intercropping systems are popular in the north, northwest, and southwest of China and often
result in yield increases compared to monocropping. Rhizosphere interactions may play a significant role in the yield increases,
particularly with respect to nutrient availability. The aim of this study was to investigate the effects of intercropping
on N availability and community composition of ammonia-oxidizing bacteria in the rhizosphere of wheat, maize, and faba bean
at different growth stages. Denaturing gradient gel electrophoresis (DGGE) based on 16S rRNA genes was used to analyze the
community composition of bacterial ammonia oxidizers belonging to β-proteobacteria. The results showed that intercropping
with faba bean significantly increased nitrate concentrations in the rhizosphere of wheat and maize at the second sampling
time (20 June) compared to monocropping or intercropping between maize and wheat. Intercropping significantly affected the
community composition of ammonia-oxidizing bacteria in the rhizosphere compared to monocropping, and the effects were most
pronounced in the maize/faba bean and wheat/maize intercropping systems when faba bean and wheat were at anthesis and maize
was in seedling stage. In wheat/faba bean intercropping, the effects of intercropping on community composition of ammonia-oxidizing
bacteria were less pronounced at the seedling stage of the two species but were significant at anthesis. 相似文献