The critical soil P levels for crop yield, soil fertility and environmental safety in different soil types

Background and aims

Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P losses and associated eutrophication of surface waters. The aim of this study was to determine critical soil P levels for achieving optimal crop yields and minimal P losses in common soil types and dominant cropping systems in China.

Methods

Four long-term experiment sites were selected in China. The critical level of soil Olsen-P for crop yield was determined using the linear-plateau model. The relationships between the soil total P, Olsen-P and CaCl₂-P were evaluated using two-segment linear model to determine the soil P fertility rate and leaching change-point.

Results

The critical levels of soil Olsen-P for optimal crop yield ranged from 10.9 mg kg^?1 to 21.4 mg kg^?1, above which crop yield response less to the increasing of soil Olsen-P. The P leaching change-points of Olsen-P ranged from 39.9 mg kg^?1 to 90.2 mg kg^?1, above which soil CaCl₂-P greatly increasing with increasing soil Olsen-P. Similar change-point was found between soil total P and Olsen-P. Overall, the change-point ranged from 4.6 mg kg^?1 to 71.8 mg kg^?1 among all the four sites. These change-points were highly affected by crop specie, soil type, pH and soil organic matter content.

Conclusions

The three response curves could be used to access the soil Olsen-P status for crop yield, soil P fertility rate and soil P leaching risk for a sustainable soil P management in field.     

长期施肥对黑土大豆根瘤菌群体结构和多样性的影响

为揭示长期施肥对黑土大豆根瘤菌群体结构和多样性的影响,采用BOX-PCR、IGS-PCR-RFLP和16S r DNA基因序列分析法,对分离自黑龙江省7种长期不同施肥处理的254株大豆根瘤菌进行了遗传多样性和系统发育分析,结合土壤理化性质分析了大豆根瘤菌群体结构和多样性与土壤因子间的关系。7种处理分别为不施肥(CK)、有机肥(OM)、单施氮肥(N1)、单施2倍氮肥(N2)、氮肥+有机肥(N1+OM)、氮肥磷肥混施(N1P1)和2倍氮肥磷肥混施(N2P2)。系统发育分析结果表明,所有供试菌株均为慢生根瘤菌属(Bradyrhizobium),其中大部分菌株与日本慢生大豆根瘤菌(Bradyrhizobium japonicum)相似性最高,少部分菌株与辽宁慢生大豆根瘤菌(Bradyrhizobium liaoningense)相似性最高。BOX-PCR聚类分析结果表明,供试菌株在70%相似性水平上分为15个群,在与施肥处理相关性分析中分为3个群体,分别对应于不施化肥处理(CK和OM)、化学氮肥处理(N1、N2、N1+OM)、氮肥磷肥处理(N1P1和N2P2)。典范对应分析结果表明,土壤p H、速效氮和速效磷与根瘤菌群体结构相关性极显著(P=0.002,0.004,0.002)。不同施肥措施下大豆根瘤菌的多样性有明显差异:N2P2处理的丰富度指数和Shannon-Wiener指数显著高于其他处理;OM处理的Simpson指数最高;N1和N2处理的3种多样性指数都显著低于其他处理。通径分析结果表明,p H、速效磷对多样性指数有较高的直接正效应;速效氮通过p H的间接负效应影响多样性指数。本研究表明,长期施用化肥改变了根瘤菌群体结构,单施氮肥减少大豆根瘤菌多样性,而氮肥磷肥混施则有助于提高大豆根瘤菌多样性。     

Differential effects of grazing,water, and nitrogen addition on soil respiration and its components in a meadow steppe

Background and aims

Understanding the influences of environmental variation and anthropogenic disturbance on soil respiration (R_S) is critical for accurate prediction of ecosystem C uptake and release. However, surprisingly, little is known about how soil respiration and its components respond to grazing in the context of global climate change (i.e., precipitation or nitrogen deposition increase).

Methods

We conducted a field manipulative grazing experiment with water and nitrogen addition treatments in a meadow grassland on the Songnen Plain, China, and assessed the combined influences of grazing and global change factors on R_S, autotrophic respiration (R_A), and heterotrophic respiration (R_H).

Results

Compared with the control plots, R_S, R_A and R_H all exhibited positive responses to water or nitrogen addition in the wet year, while a similar effect occurred only for R_H in the dry year. The responses of R_S to precipitation regimes were dominated by both frequency and amount. However, grazing significantly inhibited both soil respiration and its components in all subplots. Further analysis demonstrated that the plant root/shoot ratio, belowground biomass and microbial biomass played dominant roles in shaping these C exchange processes.

Conclusion

These findings suggest that changes in precipitation regimes, nitrogen deposition, and land utilization may significantly alter soil respiration and its component processes by affecting local carbon users (roots and soil microorganism) and carbon substrate supply in meadow steppe grasslands. The future soil carbon sequestration in the studied meadow steppe will be benefited more by the moderate grazing disturbance.

     

Bacillus daqingensis sp. nov., a halophilic,alkaliphilic bacterium isolated fromSaline-sodic soil in Daqing,China

An alkaliphilic, moderately halophilic, bacterium, designated strain X10-1^T, was isolated from saline-alkaline soil inDaqing, Heilongjiang Province, China. Strain X10-1^T was determined to be a Gram-positive aerobe with rod-shaped cells. The isolate was catalase-positive, oxidase-negative, non-motile, and capable of growth at salinities of 0–16% (w/v) NaCl (optimum, 3%). The pHrange for growth was 7.5–11.0 (optimum, pH 10.0). The genomic DNA G+C content was 47.7 mol%. Itsmajor isoprenoid quinone was MK-7 and its cellular fatty acid profile mainly consisted of anteiso-C_15:0, anteiso-C_17:0, iso-C_15:0, C_16:0, and iso-C_16:0. The peptidoglycan contained meso-diaminopimelic acid as the diagnostic diamino acid. The predominant polar lipids were diphosphatidylglycerol, phosphatidylethanolamine, and phosphatidylglycerol. Phylogenetic analysis based on 16S rRNA gene sequences showed that X10-1^T is a member of the genus Bacillus, being most closely related to B. saliphilus DSM15402^T (97.8% similarity) and B. agaradhaerens DSM 8721^T (96.2%). DNA-DNA relatedness to the type strains of these species was less than 40%. On the basis of the phylogenetic, physiological, and biochemical data, strain X10-1^T represents a novel species of the genus Bacillus, for which the name Bacillus daqingensis sp. nov. is proposed. The type strain is X10-1^T (=NBRC 109404^T = CGMCC 1.12295^T).     

自噬标志分子ATG8同源蛋白的生物信息

自噬是细胞重要的代谢途径,ATG8在自噬体形成过程中起着重要的作用。对ATG8蛋白进行生物信息学分析研究十分必要。本研究以NCBI中人ATG8同源蛋白序列数据为研究材料,分析其与10种模式生物间基因拷贝数、氨基酸序列、蛋白质保守位点相关性。结果表明,人6种ATG8同源蛋白分别定位于5条染色体上,均有泛素样GABARAP结构域。并且,所有模式生物的ATG8同源蛋白中N-端氨基酸序列保守性强于C-端序列。本研究构建的ATG8同源蛋白系统发育树显示,人的ATG8同源蛋白与脊椎动物(斑马鱼,爪蟾,小鼠,大鼠,牛)的ATG8蛋白亲缘关系更近,人的GABARAPs与酵母的ATG8蛋白与的亲缘关系较近。本研究为研究细胞自噬过程及机制提供了丰富的生物进化和生物信息数据支持。     

小兴安岭5种林型土壤呼吸时空变异

原始阔叶红松林、谷地云冷杉林、阔叶红松择伐林、次生白桦林、人工落叶松林是小兴安岭乃至东北地区的重要森林类型。采用红外气体分析法比较测定了这几种森林类型的土壤呼吸及其相关环境因子,分析探讨了这几种森林类型土壤呼吸的时空变异。结果表明:各林型土壤呼吸与5 cm深土壤温度(T5)呈显著的指数相关,并且土壤呼吸与土壤温度、土壤湿度及其相互作用的回归模型可以解释各林型土壤呼吸约71%的季节变异。生长季平均土壤呼吸速率为次生白桦林(3.59μmolCO.2m-.2s-1)>谷地云冷杉林(3.52μmolCO.2m-.2s-1)>阔叶红松择伐林(3.44μmolCO.2m-.2s-1)>原始阔叶红松林(2.58μmolCO.2m-.2s-1)>人工落叶松林(2.29μmolCO.2m-.2s-1),说明土壤呼吸对原始阔叶红松林人为干扰的响应是不同的。各林型Q10值介于1.84(人工落叶松林)—2.32(次生白桦林)之间。在整个生长季,各林型之间土壤呼吸的变异系数变化幅度为19.74%—37.39%,而各林型内土壤环间其变化幅度为32.13%—60.20%,显著大于样地间的变化幅度14.28%—35.70%(P<0.001),说明土壤呼吸在细微尺度上的差异更大。土壤湿度可以解释各林型(阔叶红松林除外)内部土壤呼吸15.8%—33.5%的空间异质性。