三江源区四种栽培禾草抗寒性研究

通过对质膜相对透性、渗透调节物质、内源保护酶系等生理生化指标的测定,对三江源区引种栽培的4种禾草:青海草地早熟禾,青海冷地早熟禾,青海中华羊茅和无芒雀麦的抗寒性进行了研究。通过综合指标判定,4种牧草的抗寒能力为青海草地早熟禾最强,然后依次是青海冷地早熟禾,青海中华羊茅,无芒雀麦的最弱。     

大同市农田杂草调查及防治

对大同市所辖农业 7县 2区的农田进行杂草调查 ,得知全市农田有杂草 16 2种 ,隶属 34科 ;划分出了北坡丘陵区、南山区、平川区及盆地灌区 4种地形型杂草 ;并就调查结果进行了分析 ,提出了防治建议     

Interrelations of vegetal cover,silicophytolith content and pedogenesis of Typical Argiudolls of the Pampean Plain,Argentina

Knowledge of the origin, evolution and weathering of Pampean soils is still limited. There are few prior studies of silicophytoliths, even though they could be important pedogenetic indicators that provide information about the role of amorphous silica in the reestablishment of soil structure. The aim of this work is to determine the silicophytolith content in Typical Argiudolls of the Pampean Plain, Argentina, its relation with vegetal cover and its effect on pedogenesis. We worked in three plots with different vegetal cover: grasses and shelter-belt plantations of Acacia melanoxylon – Celtis tala and Eucalyptus globulus – Celtis tala. In the study area, morphological characterization and particle size distribution analysis of soils were completed, and pH and organic matter content were determined. The heavy liquid separation was realized with sodium polytungstate (δ = 2.3 g/cm³) and an average of around 500 mineral grains were counted under optical microscope for the quali-quantitative analysis. There were no differences between profiles with respect to their morphological properties, organic matter content and particle size distribution, except for the higher organic horizon development of the forest plots as compared with the grass plot. The silicophytolith content was higher in the forest plots than in the grass one; within each profile, this fraction content decreased from the surface (63–40%) to the subsurface levels (23–5%) of soils. This decrease parallels the pieces of amorphous silica (< 7.5 μm) distribution in all plots analyzed. Afforestation over the past 50 years does not affect either the morphological or the physico-chemical properties of soils. These forest species, through the organic horizons, preserve soil conditions, which insures a higher representativity of silicophytoliths in comparison with the grass plot.     

十种禾草耐寒性的比较研究

通过对十种禾草半致死温度与越冬率的测定,利用最长距离聚类分析方法对其耐寒性进行了综合分析.结果表明,在北京地区耐寒性较强的禾草是草地雀麦、无芒雀麦、苇状羊茅、沙生冰草、长穗偃麦草和猫尾草,耐寒性中等的是紫羊茅、蓝茎冰草和鸭茅,耐寒性最弱的禾草为草芦.     

Impact of Fire on Soil Nitrogen Forms in Central Semiarid Argentina

Burning effects on soil N are particularly important in the Caldenal region of Argentina because N is likely to be limited and is easily lost by volatilization during fire. Burning may cause an initial increase in the mineral N content of the surface soil and, perhaps more important, can reduce the proportion of N in hydrolyzable (that is, more mineralizable) forms. The modification in soil N fractions by fire is directly related to the degree of soil heating and to the proportion and amount of N fractions remaining in the ash. This research was aimed at studying the effects of a controlled burn on total N, inorganic (NO3 and NH4+) and organic (amino acids, ammonium, hexosamines) N forms, as well as hydrolyzable and nonhydrolyzable N compounds of top soils of the southern Caldenal. Soil samples were taken from beneath the canopy of shrubs and from the areas with herbaceous cover, before and after burning. In order to show that a greater proportion of N added to regularly burned soils will result in lower levels of mineralizable N, differences in the changes of the various pools of plant tissue N upon burning at different ignition tem peratures are also reported. The initial unburned top soils had no significant differences in total, inorganic, and organic N form concentrations between shrub and herbaceous vegetation-covered soil. Burning did not affect the net content of total N in soil under woody vegetation, but in the grassland soil a decrease of total N concentration was observed. Nitrate concentration increased and NH4+ concentration decreased in both shrub and grassland soils after burning. Controlled burning caused losses of amino acid and ammonium organic N forms from the soil under grass plants and gains of hexosamine N in both shrub-and herbaceous-coveredsoils. There was an observed tendency to increase the relative proportions of non hydrolyzable N forms in both the shrub and grassland soils after burning. Inorganic and organic N form concentrations were similar in initial shrub litter and grass, but litter had higher concentrations of total and nonhydrolyzable N than those of grass. Shrub litter ash obtained after muffling at 300 C contained higher NH4+-N, aminoacid N, ammonium N, and total and nonhydrolyzable N concentrations than those from grass. An increase of 100 C in the ignition temperature produced clear ashes, rich in mineral N with little concentration of total N and C. The organic N forms affected most by the ignition temperature increase were amino acid N and ammonium N, respectively, particularly in woody litter. The most striking feature was the constituent increase in the percentages of nonhydrolyzable N forms of the vegetation covers on passing from initial to 300 C to 400 C, particularly for the litter and its ashes. These results suggest that the soil mineralizable N pool may be reduced by frequent burning or by more severe burning than observed presently in the Caldenal region.     

几种禾草的开花习性

研究１１份禾草种质料的开花习性表明：稗草，长叶雀稗及草芦的小花开放顺序，通常由顶部向基部开放，而庐山草芦及鸭茅则表现为由中上部位向上，下两端开放。单个花序开花持续时间在７－３２天。除草芦外，其余各属饲草的不同草种间小花开部特点相似。３种稗草有部分不花闭颖返粉结实。庐山草芦一日开花高峰在下午１４－１５时，其余均在上午，多数在８－１０时。     

火烧对典型草原改良的效果

本文研究了秋季火烧和春季火烧对内蒙古草原地带的羊草草原总产量优势种群羊草、大针茅以及小叶锦鸡儿数量与生长状况的影响。自１９９０年秋至１９９２秋经过两年的监测、统计与分析，主要研究结果如下：草场的总产量受大气降水的制约，火烧前后草场的总产量基本上保持稳定，中常年景的地上生物量变化在１８０──２００克／平方米之间。火烧对优质根茎禾草一羊草的增长有显著的促进作用，在生长季的中后期，火烧地段上羊草种群的地上生物量比未烧地段高出５０──９０克／平方米，提高了６００──１６０％。火烧地段上豆科草的产量略有提高，而葱类植物的产量基本上保持稳定。火烧可以抑制大针茅、小叶锦鸡儿和菊科杂类草的生长，减少它们的数量，其中以秋季火烧最为明显。在对照群落中，大针茅的产量为３０──５０克／平方米，小叶锦鸡儿为２０──５０克／平方米，火烧之后大针茅的产量减至１０──２５克／平方米，减少了５０──６０％，小叶锦鸡儿的产量一般低于１０克／平方米。火烧对草场的效应与各种植物的生活型、生长型、种群生态位（对水分和养分等资源利用情况）等特点紧密相关。火烧对草原土壤理化性质的影响也是有关因素。综上所述，有计划的火烧可以提高草群质量和利用价值，是一种?     

小麦白粉菌寄主范围研究初报

人工接种及田间调查的结果表明，采自河南和陕西的小麦白粉菌系能正常地侵染７属２３种禾本科植物。其中有６属１１种禾草为国内首次报道的该菌寄主。连同前人的研究，目前发现的我国小麦白偻菌寄主植物已达１０属３１种。从小麦属各植物材料对小麦白粉菌的感染情况，进一步支持了小麦属的现代分类理论。     

Breeding winter hardy grasses

Summary Perennial grasses are vital for Norwegian agricultural production. The nature and extent of winter damage on grasslands is highly dependent on climatic conditions, and determines both persistency and yield. Physical stresses such as frost and ice encasement predominate in coastal regions with an unstable winter climate, while biotic stresses such as low temperature fungi are more common in the inland regions. Development of hardening depends on plant adaptation and climatic conditions during autumn and winter. New winter-hardy cultivars should be bred for wide adaptation to winter stresses. The genetic background for the most important character, freezing tolerance, seems to be of polygenic nature with mainly additive gene action. Selection for increased freezing tolerance has been effective over generations in grasses, and in most grass species ample variation still exists to be exploited by breeding. However, in some species like perennial ryegrass, modern biotechnological methods should be used to improve freezing tolerance and winter hardiness.     

Critical review of the impact of cover crops on soil properties

Grasses as well as leguminous and non-leguminous broadleaves are the major categories of commonly grown cover crops worldwide. This review focuses on the contribution of cover crops to soil properties. The review first considers the single and mixed cover crops and shows that grass species are desirable for their decay and ability to provide substantial soil cover, broadleaf species are used for their quick decomposition and capacity of releasing residues into the soil, while the leguminous species are used for their ability to fix atmospheric nitrogen. Secondly, the impacts of cover crops on soil health are reviewed. Integrating cover crops into conventional cropping systems may reduce soil bulk density, improve soil structure and hydraulic properties to facilitate increased water infiltration and storage. Crop residue additions from cover crops may enhance soil organic C and N accretion as well as increase availability of P, K, Ca, Fe and Mg in some soil types under certain climatic conditions. Further, cover crops may provide a better condition for microbial activity, abundance, and diversity. Finally, the review shows that through proper management, cover crops may be utilized as an essential component of soil conservation practices for enhanced soil health. Still, further investigation is necessary to determine cover crop effects in additional cropping systems and climatic zones as well as the long-term effects of cover crops on soil properties, subsequent crop yield, and overall cropping system profitability. This review is an important source of information for crop growers, crop management institutions, universities, and crop consultants for sustainable agricultural production.