Cd2+胁迫对紫花苜蓿叶绿素和可溶性糖含量的影响

以紫花苜蓿为试材,采用盆栽试验,研究不同浓度Cd2 胁迫对不同茬期紫花苜蓿的叶绿素、可溶性糖的影响。结果表明:随重金属Cd2 胁迫剂量的加大,3茬紫花苜蓿叶绿素含量、可溶性糖含量呈倒"N"形规律变化,即降-升-降的变化,这与重金属诱导下紫花苜蓿的防御机制有关。3茬紫花苜蓿的可溶性糖含量不同,依次是第1茬>第2茬>第3茬,3茬紫花苜蓿的叶绿素含量不同:低浓度Cd2 下,第2茬>第1茬>第3茬;高浓度Cd2 下,第2茬>第3茬>第1茬。主要原因可能是由于苜蓿的收割,导致Cd流失,胁迫作用减弱或者是多种影响因素综合作用的结果。     

低温层积过程中圆齿野鸦椿种子的生理生化变化

通过对不同层积时间圆齿野鸦椿种子萌发及其生理生化变化情况的研究,得出种皮对圆齿野鸦椿种子萌发具有很强的机械障碍,仅通过低温层积不能完全解除种皮的机械障碍.低温层积配合60℃温水浸种能够有效解除休眠.同时通过实验发现,当采取播前温水处理打破种皮机械障碍时,以低温层积90～120 d为宜,层积时间过长会导致萌发率降低.通过实验,对低温层积不同时间的圆齿野鸦椿种子生理生化变化情况进行测定,结果表明:随着层积时间增加,可溶性糖含量与G-6-PDH和6-PGDH联合酶活性波动上升,而淀粉含量波动下降.说明种子内含物质相互转化,逐步解除休眠,同时种子呼吸代谢中戊糖磷酸途径所占比重上升.POD活性先逐渐上升,在120 d后活性下降,笔者认为这可能是导致层积120 d后种子萌发率降低的主要原因.     

Natural variation within the genus Beta and its possible use for breeding sugar beet: A review

Summary Sugar beet is a relatively young crop, which supposedly has a narrow genetic base. Natural variation occurring in primitive beet varieties and in wild Beta species has been used for breeding sugar beet. This paper reviews information on desirable characteristics in Beta germplasm and the attempts made for the introgression of such characters into commercial breeding material. After an introduction on the availability of germplasm and the possibilities of hybridisation, attention is focussed on the mating system (especially male sterility), on morphological and physiological characteristics, including yield and sugar content, and on resistances to diseases and pests.     

The effect of accidental selfing on the analysis of a diallel cross with sugar cane

Summary The diallel cross was found to be an unsuitable design for quantitative genetic analyses with sugar cane.Accidental selfing caused substantial inbreeding depression for most characters. Consequently, analysis of a diallel cross without regard to the effect of accidental selfing would be subject to bias, if accidental selfing were common. A selfing model proposed by Dudley (1963) was extended to include differential selfing, and was tested in an experiment in which the percentage of selfing in each cross was estimated visually.Variance components had large standard errors, which prevented firm conclusions from being drawn, but selfing appeared to cause substantial bias in the estimates. Estimates of genetic variance components from a p(p-1) diallel set, using the extended selfing model, were compared with estimates obtained from the standard analyses in which reciprocal or maternal effects should account for the effect of selfing. The estimates were comparable, but the standard analyses were simpler and produced estimates with lower standard errors.When the effects of selfing were minimized, general combining ability (g.c.a.) effects appeared to be much more important than specific combining ability (s.c.a.) effects for most characters.     

苦荞提取物对大小鼠血糖、血脂的调节

试验观察了苦荞提取物对四氧嘧啶所引起的高血糖型大鼠的降血糖作用及对高血脂症动物血脂的影响。结果表明，苦荞提取物对正常大鼠血糖无影响，大、中剂量对四氧嘧啶所致的高血糖大鼠空腹血糖有明显的降低作用，并改善由四氧嘧啶所引起的高血糖大鼠的糖耐量。给予大剂量苦荞提取物可使大鼠血清总胆固醇（TC）浓度显著下降，给予中剂量可使大鼠血清甘油三酯（TG）浓度显著下降。     

不同浓度盐胁迫对转基因饲用甜菜种子萌发及幼苗生长的影响

通过不同浓度NaCl溶液处理转基因饲用甜菜种子及其幼苗试验，研究了盐胁迫下种子萌发、幼苗生长及胁迫解除后种子的效应，为盐土农业生产提供理论依据。结果表明，转基因饲用甜菜种子萌发的适宜Nacl浓度为50。150mmol/L，其中100mmoL／LNaCl胁迫下，种子发芽率最高，与对照相比高6．78％。随着盐胁迫浓度的升高，种子萌发延迟，萌发率也呈不同程度的降低。盐胁迫解除后，种子萌芽迅速，萌芽率提高，整齐度增加。转基因饲用甜菜幼苗在不同NaCl浓度胁迫下表现出的反应不同，高盐胁迫对抑制幼根生长影响较大。     

气象条件对酿酒葡萄若干品质因子的影响

根据2004-2005年北方6省酿酒葡萄主要产区葡萄取样和宁夏芦花台园艺场田间试验资料，分析了影响酿酒葡萄主要品质因子总糖、总酸、pH值和单宁积累的气象因子和影响时段，并建立了关系模式，提出了影响酿酒葡萄品质的定量气象指标。研究结果表明：酿酒葡萄品质与气象条件密切相关，主要影响因子是降水量、积温和气温日较差等。影响酿酒葡萄品质形成的关键时期是7-8月（幼果膨大-果实着色期），其次是果实着色期-成熟期。7—8月降水量和水热系数对酿酒葡萄总糖含量的影响最大，7-8〉130mm，K7-8〉1．62时，总糖含量不能达到170g／L（酿优质酒所需最低糖度）。酿酒葡萄总酸含量与果实采收前一个月水热系数呈幂指数关系，随水热系数增加，含酸量缓慢增加。因此，要使酿酒葡萄果实中酸含量达到5～6g／L，则果实采收前一个月的水热系数应在0．12～0．63。酿酒葡萄中单宁含量与开花-成熟期积温、8月平均气温、9月l日到果实采收期日较差和采收前一个月平均最低气温呈指数关系，与8月日照时数呈二次曲线关系。酿酒葡萄果实的pH值随开花-成熟期平均最高气温和果实膨大期蒸发量的增加而增加。     

Boron fertilization improves seed yield and harvest index of Camelina sativa L. by affecting source-sink

The impact of soil (1, 2 kg ha^?1) and foliar (100, 200 mg L^?1) boron (B) with control (no B) was evaluated on phenology and yield formation of Camelina each applied at stem elongation and flowering stages. Foliar (200 mg L^?1) or soil B (2 kg ha^?1) resulted in earlier flowering and maturity, increased fruit bearing branches (19.68%), number of siliqua, seeds per siliqua (4.6%), biological yield (15%), seed yield (24%), harvest index (11.4%) and oil contents (23%) than no B. Increased fruit bearing branches, seed filled siliqua or seed numbers, harvest index and oil quality can be attributed to changes in dry matter accumulated of stem with simultaneous increase in siliqua dry weight with foliar or soil applied B. In crux, foliar (200 mg L^?1) or soil applied (2 kg ha^?1) B seems promising to improve seed and oil yield, harvest index of Camelina sativa under B deficient condition.     

Organic C and N stabilization in a forest soil: Evidence from sequential density fractionation

In mineral soil, organic matter (OM) accumulates mainly on and around surfaces of silt- and clay-size particles. When fractionated according to particle density, C and N concentration (per g fraction) and C/N of these soil organo-mineral particles decrease with increasing particle density across soils of widely divergent texture, mineralogy, location, and management. The variation in particle density is explained potentially by two factors: (1) a decrease in the mass ratio of organic to mineral phase of these particles, and (2) variations in density of the mineral phase. The first explanation implies that the thickness of the organic accumulations decreases with increasing particle density. The decrease in C/N can be explained at least partially by especially stable sorption of nitrogenous N-containing compounds (amine, amide, and pyrrole) directly to mineral surfaces, a phenomenon well documented both empirically and theoretically. These peptidic compounds, along with ligand-exchanged carboxylic compounds, could then form a stable inner organic layer onto which other organics could sorb more readily than onto the unconditioned mineral surfaces (“onion” layering model).To explore mechanisms underlying this trend in C concentration and C/N with particle density, we sequentially density fractionated an Oregon andic soil at 1.65, 1.85, 2.00, 2.28, and 2.55 g cm⁻³ and analyzed the six fractions for measures of organic matter and mineral phase properties.All measures of OM composition showed either: (1) a monotonic change with density, or (2) a monotonic change across the lightest fractions, then little change over the heaviest fractions. Total C, N, and lignin phenol concentration all decreased monotonically with increasing density, and ¹⁴C mean residence time (MRT) increased with particle density from ca. 150 years to >980 years in the four organo-mineral fractions. In contrast, C/N, ¹³C and ¹⁵N concentration all showed the second pattern. All these data are consistent with a general pattern of an increase in extent of microbial processing with increasing organo-mineral particle density, and also with an “onion” layering model.X-ray diffraction before and after separation of magnetic materials showed that the sequential density fractionation (SDF) isolated pools of differing mineralogy, with layer-silicate clays dominating in two of the intermediate fractions and primary minerals in the heaviest two fractions. There was no indication that these differences in mineralogy controlled the differences in density of the organo-mineral particles in this soil. Thus, our data are consistent with the hypothesis that variation in particle density reflects variation in thickness of the organic accumulations and with an “onion” layering model for organic matter accumulation on mineral surfaces. However, the mineralogy differences among fractions made it difficult to test either the layer-thickness or “onion” layering models with this soil. Although SDF isolated pools of distinct mineralogy and organic-matter composition, more work will be needed to understand mechanisms relating the two factors.