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1.
为建立‘哈伯’南天竹组织培养和种苗繁育技术体系,以半木质化带芽茎段为外植体材料开展植株再生研究。通过观察对比试验法、L9(34)正交试验设计完全随机法、极差分析、显著性检验、LSD多重比较,探讨了‘哈伯’南天竹组培的最适培养基配方。试验结果表明:最佳诱导培养基为MS + 6-BA 2.0 mg/L + IBA 0.1 mg/L +蔗糖30 g/L,诱导萌动率71.77%,成活率85.51%;最佳增殖培养基为WPM +6-BA 1.5 mg/L + IBA 0.01 mg/L + 蔗糖30 g/L,增殖系数6.3;最佳生根培养基为1/2 MS+ IBA 0.5 mg/L + NAA 1.0 mg/L + 蔗糖20 g/L + AC 0.2 g/L,生根率97.63%;试管苗移入泥炭土:珍珠岩=3:2(V/V)混合基质中,移栽成活率96.67%。该试验建立了高效稳定的组培快繁技术体系,得到的组培苗后代能够稳定的保持母本优良性状,为工厂化育苗提供了技术支撑。 相似文献
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杉木种子园为培育高产稳产杉木良种提供重要保障,在林业生产中具有积极意义。通过试验研究,探究杉木3代种子园土壤养分丰缺情况、养分间的平衡规律,确定杉木种子园最佳肥料配比和施肥量,以期为闽北低山丘陵红壤分布区杉木种子园提供推荐施肥配方。采用“3414”配方施肥设计方案,对闽北第3代杉木种子园开展N、P、K、Ca、Mg、B、Mo等元素施肥试验。分别设计大量元素氮、磷、钾三因素施肥水平(并增设施用钼肥处理)、中微量元素钙、镁、硼三因素施肥水平,以球果数量(质量)、出籽率、种子产量、胸径等为评价指标,拟合肥料效应函数方程,研究各养分间的作用规律,并提出最佳施肥配比和施肥量。结果表明:种子园土壤N、P、K、Ca、Mg养分含量较低,B含量属于中等水平,而Mo含量较高;N、P、Mg以及N-K、Ca-B肥料联合对种子园产量的影响达到显著或极显著水平,而单施某一肥料效应较小,其中单施K、Ca、B几乎没有效果,而肥料联合施用效果较好。综合效应分析结果,得出种子园最大产量施肥量组合为:每株施尿素100 g+过磷酸钙897 g+氯化钾150 g+石灰150 g+硫酸镁105 g+硼砂75 g,并配施钼肥。N、P2O5、K2O、CaO、Mg、B、Mo的用量依次为46.0、107.7、90.0、75.0、31.4、2.3、5.0 g,其配比为N:P2O5:K2O:CaO:Mg:B:Mo=1.0:2.3:2.0:1.6:0.7:0.05:0.1。多元素配方施肥能很好地改善杉木种子园产量和质量,单株球果产量、球果单粒重、出籽率及种子园产量等指标均比不施肥的母树有大幅度提高。本研究施肥方案,理论上种子园产量可达45.99~95.65 g/株,大量元素施肥试验的产量达到理论产量的80%~86%,中微量元素施肥试验的产量为理论产量的70%左右。现实种子园平均产量大约是预测产量的40%,通过合理配方施肥有望大幅度提高杉木3代种子园产量。 相似文献
3.
鸡的微卫星DNA标记与胴体性状的相关分析 总被引:4,自引:1,他引:3
测定了青脚麻鸡与隐性白鸡杂交后自交的F2代个体的全净堂重、全净堂率、脂肪宽带、腹脂重和腹脂率6个胴体性状,检测10个微卫星DNA标记,对标记基因型胴体性状值进行方差分析和多重比较,结果表明:MCW328对于10周龄体重和全净膛重两性状各基因型均有显著的差异(P<0.05);ADL292对于腹脂重性状各基因型有极显著的差异(P<0.01),对于腹脂率有显著的差异(P<0.05)。MCW328标记基因与控制10周龄体重和全净膛重QTL连锁,ADL292标记基因与控制腹脂重和腹脂率QTL连锁。 相似文献
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对N×特青示范田中试区与肥料试验田各处理小区稻株分析结果表明:抽穗后,亚种间杂交稻N×特青比常规稻特青干物质生产能力强,灌浆速度快;地上部各器官占植株干重比例,前者叶片比重大于茎,后者茎比重大于叶。亚种间杂交稻对肥料反应敏感,抽穗后,干物质累积,植株高度,每穗总粒数和粒重均随施肥量增加而增加,在高肥区有利于进一步提高产量,但增施氮肥后,灌浆速度明显滞后。 相似文献
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A field experiment was conducted during the winter seasons of 1992–93 and 1993–94 at Anand to study the effect of FYM, nitrogen and source of fertilizer on growth and yield of mustard [ Brassica juncea (L.) Czernj & Cosson]. The results showed significant variation in leaf area index (LAI), crop growth rate (CGR), dry matter production and seed yield. The direct effect of farmyard manure (FYM) was conspicuous in improving the growth of mustard. FYM application at 10 tonnes ha−1 significantly increased the LAI, CGR and dry matter accumulation per plant at almost all the stages during first year study (1992–93) and in pooled analysis. Similarly, nitrogen application registered maximum LAI, CGR at 75 kg level and RGR and NAR at 50 kg level at almost all the during both years. Sulphur carrying source (Ammonium sulphate plus single super phosphate) increased all stages growth characters. Maximum dry matter accumulation per plant and seed yield were recorded with highest levels of FYM (20 tonnes ha−1 ), N (75 kg ha−1 ) and source having S. Seed yield was strongly associated with LAI and dry matter accumulation per plant at all the stages. 相似文献
9.
Abstract. Usual residue-management options are to remove the residue, use it as mulch with or without undercutting or to incorporate it into the soil. While the role of surface mulch in evaporation has been widely studied, the information on the effect on evaporation of mulch with undercutting or residue incorporated into soil, particularly in relation to soil type and evaporativity (Eo) is lacking. We studied the effect of wheat straw used in various ways on the course of evaporation loss from soil columns with three soils at Ludhiana, India and one soil at Bushland, Texas, USA, under two Eo's Energy-limited evaporation rates under mulch (Eom) followed the soil-specific relation Eom/Eo= a e(bRes+cEo), where Res is residue rate t/ha and a, b and c are constants; Eo, is expressed in mm/d. In an effort to model the total evaporation (CE) during the energy-limited stage ‘U’ was obtained from appropriate CE versus time curves and (CE-U) was regressed over (t - ti)0.5 to obtain the slope ‘α’ (Ritchie 1972) for the soil-limited evaporation stage. The observed ‘U’ was independent of mulch rate and Eo but was strongly affected by soil type, Values of ‘α’ decreased with increase in mulch rate and decrease in Eo and coarseness of soil. The otherwise short lived benefit of evaporation reduction with mulch per se, which peaked after a few days was maintained when residue was mixed with soil at the stage when evaporation reduction reached a maximum; this benefit continued for several weeks. Cumulative evaporation values computed from ‘U’ and ‘α’ agreed closely with the observed values under straw mulch for loamy sand and clay loam soils and for ‘undercut’ and ‘residue mixed’ treatments on all soils regardless of Eo, and for all situations under small Eo. However, for sandy loam and silt loam soils under Eo of 10 mm/d, the modified square root of the time function of Jalota et al. (1988) gave a better fit. 相似文献
10.