通辽地区美国白蛾发生规律及防治对策初探

通过对通辽地区2016-2019年气温的调查统计得知:超过10℃的天数主要集中在3-11月,分别为174天、176天、182天、175天;超过10℃的有效积温分别为1 728.1日度、1 743.9日度、1 761.4日度、1 731.1日度;根据美国白蛾完成1个世代所需要的有效积温可知,发生代数分别为1.95代、1.97代、1.99代、1.96代;故通辽地区属于2代区。     

芥菜吸收积累重金属研究进展

指出了土壤重金属污染状况和由此导致的蔬菜重金属污染风险不容忽视。针对不同品种芥菜吸收和积累重金属的特性、吸收机制以及应用方面进行了综述,为研究芥菜吸收积累重金属的机理和应用提供参考。     

施肥对春青稞干物质积累、分配及产量的影响

为研究施肥对青稞干物质积累、分配及产量的调节作用,以‘藏青27’、‘QTB13’和‘QTB25’为试验材料,比较分析不同施肥处理下干物质积累、分配及产量的变化规律。结果表明：增加施肥量促进青稞分蘖期—成熟期的干物质积累及开花期和成熟期干物质向营养器官和籽粒的分配,提高了花前营养器官贮藏同化物转运量及对籽粒贡献率,降低了花后同化物输入籽粒量对籽粒贡献率。‘QTB13’和‘QTB25’在F₂条件下,更有利于干物质积累及向营养器官和穗部的分配,花后同化物输入籽粒量最大,产量也最大。‘藏青27’在F₃条件下,更有利于干物质积累及向营养器官和穗部的分配,花后同化物输入籽粒量和对籽粒贡献率最大,产量也最大。说明合理施肥有利于青稞干物质积累分配及产量提高。     

玉米秸秆消化率全基因组关联分析

48h体外干物质消化率（48h in vitro dry matter digestibility, 48h IVDMD）是衡量青贮玉米品质的重要指标。为了初步探究玉米秸秆消化率的分子遗传机理,以341份玉米自交系为材料,于2018年在沈阳和通辽种植,收获后测定秸秆48h IVDMD。利用全基因组重测序获得的6 276 612个高质量SNPs进行全基因组关联分析,共检测到153个与玉米秸秆消化率显著相关的SNPs位点（P<1.0×10^-6）,4个SNPs显著水平在P<1.0×10^-8以上;共找到38个秸秆消化率的候选基因,主要涉及细胞生长发育、防御反应和信号转导等生物学功能。     

滴灌模式和水分调控对夏玉米干物质和氮素积累与分配及水分利用的影响

采用裂区试验设计探究了地下滴灌和地表滴灌(drip underground, DU; drip surface, DS)模式下土壤水分调控(分别为田间持水量的40%～50%、60%～70%和80%～90%,记为W40、W60和W80)对夏玉米干物质和氮素积累与分配及水分利用效率的影响。结果表明,DU处理的吐丝后氮素积累量及水分利用效率分别较DS显著提高了6.18%和4.85%～8.61%。夏玉米的干物质、氮素指标及产量对滴灌模式的响应依赖于土壤水分调控水平,在W40和W60处理条件下,DU处理显著增加夏玉米的净光合速率,提高了吐丝后干物质和氮素的积累量及向籽粒的转运,最终DU处理的干物质积累量、籽粒氮素积累量、产量及氮肥偏生产力分别提高了3.29%～19.94%、?1.10%～20.65%、3.29%～19.94%和3.31%～23.64%。而在W80处理条件下, DS处理的干物质积累量、吐丝后氮素积累量、产量及蒸散量比DU处理分别提高了6.80%～12.24%、5.93%、8.39%～14.91%和9.73%～14.57%。综上所述,在限水灌溉条件下,地下滴灌能够增加吐丝后干物质积累量、氮素积累量及其对籽粒氮素的贡献率,最终增加产量。在充分供水条件下,地表滴灌更有利于干物质及氮素的积累,但由于消耗过多的水分,因此水分利用效率未显著增加。     

Agronomic performance of winter wheat grown under highly divergent soil moisture conditions in rainfed and water‐managed environments

Even in the temperate climates of Europe, increasing early season drought and rising air temperature are presenting new challenges to farmers and wheat breeders. Sixteen winter wheat (Triticum aestivum L.) genotypes consisting of three hybrids, six line cultivars and two breeding lines from Germany as well as five line cultivars from France, Austria, Slovakia, Hungary and the Ukraine (referred to as “exotic” lines) have been included in this study. The genetic materials were evaluated over three growing seasons under a range of soil moisture regimes at the three North German sites Braunschweig (irrigated and drought‐stressed), Warmse (rainfed) and Söllingen (rainfed). The average grain yields in the twelve growth environments (water regime × season combinations) ranged from 6.1 to 13.5 t ha^?1. The exotic lines showed little evidence of specific phenological adaptation to drought although they are frequently faced with water scarcity in their countries of origin. The hybrids and German lines exhibited higher regression coefficients (b_i) to environmental means than the exotic lines, indicating particular adaptation to favourable growing conditions. The phenotypical correlations of grain yield between the various environments were high, ranging for instance from 0.6 to 0.8 for the irrigated and drought‐stressed environments at Braunschweig. It is thus expected that in the foreseeable future continued selection aiming at high yield potential will suffice as a means to counter the expected increase in droughts.     

臭氧胁迫对不同敏感型水稻干物质积累与分配的影响

【目的】研究臭氧胁迫对不同敏感型水稻物质生产与分配的影响,为耐性水稻品种的选育提供参考。【方法】利用自然光气体熏蒸平台,以23个水稻品种或株系为供试材料,设置室内对照(臭氧浓度为10 nL/L)和臭氧浓度增高臭氧浓度为(100 nL/L)处理,研究臭氧胁迫对水稻成熟期地上部物质积累与分配的影响及其与最终生长量响应的关系。采用组内最小平方和的动态聚类方法,将所有供试材料按地上部最终生物量对臭氧胁迫的响应从小到大依次分为A、B和C三类不同敏感型水稻。【结果】与对照相比,臭氧胁迫使A、B和C类水稻成熟期地上部干质量平均分别下降19%、39%和52%,B和C类达极显著水平。臭氧胁迫使A类水稻成熟期叶片干质量略增,但使B类(–11%)、C类水稻(–25%)极显著下降。臭氧胁迫下A、B和C类水稻的茎秆和稻穗干质量均显著或极显著下降,其中茎秆干质量分别下降26%、41%和57%,稻穗干质量分别下降34%、59%和62%。臭氧胁迫使叶片占地上部干质量的比例大幅增加(+46%),而茎秆(–8%)和稻穗(–24%)占地上部干质量的比例极显著下降。臭氧处理与水稻类型对上述参数均有不同程度的交互作用,表现为A类水稻对臭氧的响应明显小于其他两类水稻。【结论】100 nL/L臭氧浓度严重影响水稻器官建成,减少光合产物向茎秆和稻穗的分配比例,但使叶片干质量比例大幅增加,臭氧熏蒸还导致茎秆机械强度明显下降。这些变化敏感水稻总体上较钝感类型水稻表现更为明显。     

青藏高原东北部3种野豌豆植物学特性及资源储量

采用野外定点法、最小样方法和统计学方法对生长于青藏高原东北部的3种野豌豆属植物的植物学特性、生态环境、群落数量特征及资源储量进行研究。结果显示,救荒野豌豆、山野豌豆和三齿萼野豌豆的植物学特性、生态环境和群落数量特征具有一定差异,3种野豌豆在青海省的资源总储量分别为0.46×10~6、0.23×10~6、0.27×10~6 kg,表明3种野豌豆属植物的资源总量在青海省并不高,应对其进行有效的引种驯化,实现人工繁育和增加资源储量,这既可保护青海省甚至青藏高原的生态环境,也可对其资源进行有效地保护和合理开发利用。     

Driving forces of soil organic matter change in Jiangsu Province of China

Soil organic matter (SOM) is a key property determining soil functions and a major form of carbon stored in soil. Understanding the spatial and temporal variability of SOM and the driving forces responsible for spatial and temporal changes is important to assess regional soil quality and carbon sequestration potential and, particularly, to establish better practices for land use and management. We evaluated the spatio‐temporal change in SOM content from 1979–1982 to 2006 and its driving forces in Jiangsu Province, East China, using geostatistics. The results showed that mean SOM content increased from 16.60 ± 8.50 to 18.31 ± 8.32 g/kg over a 26‐yr period. The maps of SOM generated by ordinary kriging represented the increasing trend from north to south across the province in the two periods. The level of SOM in 1979–1982 affected the pattern of change: the SOM increasing in areas initially with a small content while decreasing in areas having a large content. The map of SOM change showed that the rate of increase decreased from north to south within the province. Increased fertilizer application promoted crop production with more residual biomass being retained in the soil, which resulted in increased SOM content. Land use changes to paddy, upland or forest improved SOM content, whereas abandoning land reduced SOM content.     

Evaluating biodegradability of soil organic matter by its thermal stability and chemical composition

The stability of soil organic matter (SOM) as it relates to resistance to microbial degradation has important implications for nutrient cycling, emission of greenhouse gases, and C sequestration. Hence, there is interest in developing new ways to quantify and characterise the labile and stable forms of SOM. Our objective in this study was to evaluate SOM under widely contrasting management regimes to determine whether the variation in chemical composition and resistance to pyrolysis observed for various constituent C fractions could be related to their resistance to decomposition. Samples from the same soil under permanent pasture, an arable cropping rotation, and chemical fallow were physically fractionated (sand: 2000-50 μm; silt: 50-5 μm, and clay: <5 μm). Biodegradability of the SOM in size fractions and whole soils was assessed in a laboratory mineralization study. Thermal stability was determined by analytical pyrolysis using a Rock-Eval pyrolyser, and chemical composition was characterized by X-ray absorption near-edge structure (XANES) spectroscopy at the C and N K-edges. Relative to the pasture soil, SOM in the arable and fallow soils declined by 30% and 40%, respectively. The mineralization bioassay showed that SOM in whole soil and soil fractions under fallow was less susceptible to biodegradation than that in other management practices. The SOM in the sand fraction was significantly more biodegradable than that in the silt or clay fractions. Analysis by XANES showed a proportional increase in carboxylates and a reduction in amides (protein) and aromatics in the fallow whole soil compared to the pasture and arable soils. Moreover, protein depletion was greatest in the sand fraction of the fallow soil. Sand fractions in fallow and arable soils were, however, relatively enriched in plant-derived phenols, aromatics, and carboxylates compared to the sand fraction of pasture soils. Analytical pyrolysis showed distinct differences in the thermal stability of SOM among the whole soil and their size fractions; it also showed that the loss of SOM generally involved preferential degradation of H-rich compounds. The temperature at which half of the C was pyrolyzed was strongly correlated with mineralizable C, providing good evidence for a link between the biological and thermal stability of SOM.