小麦干物质积累与穗粒重形成的研究

本试验研究了11个品种(系)穗粒重形成过程中的干物质累积分配特性。小麦开花后穗粒重形成可分为初期(即穗粒形成期,开花至花后10天)、中期(花后10天至30天),和后期(花后30天至成熟)三个阶段穗粒重与中、后期的灌浆速率密切相关,其相关数分别为0.9757和0.8518后期灌浆速率存在较大的遗传变异性,可供育种家利用。本研究指出,重穗育种应在增加同化源的基础上,着重提高穗粒数。     

旱坡地集水枣园土壤水分动态研究

在旱坡地上采取隔坡集蓄径流水平沟的整地方法营建枣园，集蓄坡面径流，增加枣园土壤含水率，有效地控制水土流失；通过对枣园土壤水分连续３年的定点观测，掌握了枣园土壤水分动态的变化规律，分析结果表明，所采取的集水工程集水效果较好。     

阳坡山地花椒园的立地条件和丰产试验

阳坡山地花椒园光热充足,但土壤水分、养分条件较差,因而,限制了单株产量。采用园地覆膜、尿素叶面喷肥技术措施能明显提高单株产量,是石灰岩山地花椒园的重要增产措施。     

杉木球花特性及其种子园花粉量的研究

本文以姥山杉木初级种子园、杉木种源林和普通杉木林为对象,对杉木雌雄球花在树冠中的分布及其发育过程,雄球花特征值频率分布,雄球花大小分类及花粉产量等进行了研究。结果表明,杉木雌雄球花在树冠中的分布具有成层性。雌球花主要分布在树冠上、中部,雄球花则主要分布在下、中部。杉木雄球花及花粉特征值频率分布为偏态分布。雄球花的大小可按小孢子叶球数平均值一倍的标准差,分为大、中、小3类。花粉的客重为656.071 8mg/cm~3。用容重法测得的每个孢粉囊产生的花粉为3700粒。姥山杉木种子园平均每株母树产生花粉约697 g,约35.1亿粒。整个种子园产花粉约12681kg,约6.5478×10~(14)粒。偏雄,宜进行适当改造。     

半干旱黄土高原生物结皮处理下集水造林的初步研究(英文)

集水措施是干旱半干旱地区解决因降雨少且季节间分配不均带来的水资源短缺的主要措施之一,有关微集水区防渗处理材料及其防渗效果的研究也已广泛开展。本文通过5 年(1992-1996)的野外试验对半干旱黄土高原微集水系统生物结皮覆盖对造林的影响进行了研究。结果表明,结皮接种3 年后,集水区表面大部分为结皮所覆盖,其集水功能已经部分地表现出来。在春季3 个典型时段内浅层土壤含水量与对照相比显著提高(0.05 水平),1m 土层内春季月均含水量均比对照提高了0.9%–6.04%。同时在研究期末(1996 年)结皮处理的样地内树木个体的树高(H)、胸径(DBH)和地径(DGL)均较对照有显著提高(0.05 水平),提高幅度分别为22.38%、17.34%和20.49%。作为一种生物防渗材料,生物结皮具有无污染、自我繁殖、使用期长和投入小等特点,因此很可以作为西部大开发中植被恢复的主要集水材料,进一步的工作应放在干旱环境下当地适宜结皮种类的选择及其快速繁殖技术上。     

Do rates of litter decomposition tell us anything we really need to know?

Results of several long-term studies of non-woody litter decomposition in forests indicate that we need to rethink why and how we measure rates of litter decomposition. Effects on litter decomposition rates were postulated to explain some of the nutritional effects of factors such as tree species, forest harvesting and fertilization. However, the accumulated experimental evidence indicates that litter decomposition rates do not mediate these responses. Many studies have reported litter mass loss becoming extremely slow at values considerably below 100%, indicating that early decay rates may not accurately foreshadow the entire decay process. Exclusion of soil faunal activities from current measurements of decomposition rates seriously reduces the likelihood that we are properly modeling decomposition. Finally, the use of regression and correlation analyses to determine which climate or initial litter quality factors control decay rate has led to many unwarranted and potentially misleading conclusions. These concerns are illustrated with examples from a suite of litter decomposition studies in British Columbia, Canada. Insights into nutrient cycling and carbon storage in ecosystems are more likely to arise from measuring the mass and nutrient content of annual litter input and determining the maximum decomposition limit and nutrient content at that stage, than by measuring early rates of decay. Improved predictions of relative decay rates of plant litters are likely to arise from a holistic approach based on plant life attributes rather than correlations based on individual initial litter chemistry parameters. Finally, a better understanding of the fate of faecal material of soil fauna is necessary before we can accurately predict and model litter decomposition.     

岷江上游不同植被类型的土壤水分和物理性质

土壤水分-物理性质是衡量土壤质量的重要指标。本文测定了岷江上游理县云杉人工林、灌木林、经济林和农耕地的土壤物理性质。结果表明:(1)云杉人工林的土壤容重最小,土壤毛管孔隙度、非毛管孔隙度、田间最大持水量、毛管持水量显著高于其余3种植被类型;(2)灌木林与经济林的非毛管孔隙度、毛管持水量、田间最大持水量差异不显著,但灌木林的土壤容重显著小于经济林;(3)农耕地的土壤容重显著高于其余3种植被类型,非毛管孔隙度、毛管持水量、田间最大持水量显著低于其余3种植被类型。研究结果说明4种植被类型的土壤物理性质存在较大差异,选择合理的植被类型和减少人为干扰对于岷江上游地区植被恢复和生态功能改善具有重要的作用。     

Relationships between soil and foliar nutrients in young densely planted mini-plots of Pinus radiata and Cupressus lusitanica

The long-term nature of forest crop rotations makes it difficult to determine impacts of forestry on soil nutrients that might be depleted by forest growth. We used small scale, highly stocked plots to compress the length of the rotation and rapidly induce nutrient depletion. In the study, two species (Pinus radiata D. Don and Cupressus lusitanica Miller) are compared under two disturbance regimes (soil undisturbed and compacted), and two fertiliser treatments (nil and plus fertiliser), applied in factorial combination at 33 sites, covering the range of climatic and edaphic variation found in plantation forests across New Zealand. To assess our ability to rapidly highlight important soil properties, foliar nutrient concentrations were determined 20 months after planting. It was hypothesised that the densely planted plots, even at a young age, would create sufficient pressure on nutrient resources to allow development of relationships between properties used as indicies of soil nutrient availability and foliar nutrient concentrations. For both species significant relationships between foliar nutrients and 0–10 cm layer soil properties from unfertilised plots were evident for N (total and mineralisable N) and P (total, acid extractable, organic, Bray-2 and Olsen P). With the exception of Ca in C. lusitanica, foliar K, Ca and Mg were correlated with their respective soil exchangeable cation measures. The results thus confirm the utility of the experimental approach and the relevance of the measured soil properties for forest productivity.

In unfertilised plots foliar N and P concentrations in P. radiata exceeded those in C. lusitanica, the differences being eliminated by fertiliser application. Foliar N/P ratios in P. radiata also exceeded those in C. lusitanica. In contrast to N and P, foliar K, Ca and Mg concentrations were all higher in C. lusitanica, the difference being particularly marked for Ca and Mg. P. radiata contained substantially higher concentrations of the metals Zn, Mn and Al than C. lusitanica, whereas the latter contained higher B concentrations. Possible reasons for differences between species in foliar nutrient concentrations are discussed.     

Effects of N, NP, and NPKS fertilizers applied to four-year old hybrid poplar plantations

Mineral fertilizers were applied to adjacent plantations of 2, 4-year old, hybrid poplars: clone 27 (Northwest, P. deltoides × P. balsamifera) and 794 (Brooks, P. deltoides × P. × petrowskyana), in north eastern Alberta. Fertilization was done in May 2003 to see whether growth rates could be increased and rotations shortened. Three fertilizers (N, NP and NPKS + Cu + Zn) were applied at each of three rates (supplying N at 0, 100 and 200 kg ha⁻¹) in a factorial randomized block design to the two separate plantations. Fertilization with 200 kg ha⁻¹ N and 100 kg ha⁻¹ P increased volume growth of clone 27 by 1 m³ ha⁻¹ year⁻¹ over 2 years. Clone 794 showed no volume response to fertilization, but produced 8.7 m³ ha⁻¹ more than clone 27. Leaf area, dry mass and nutrient concentrations of both clones increased in the first year after fertilization, showing that fertilizer uptake occurred. Decrease in leaf size between 2003 and 2004 was affected by fertilizer level in clone 794. There were differences between some nutrient concentrations in the soils occupied by the two clones, and clone 794 had higher leaf concentrations of N, K, Ca, S, Mn, Zn, B and Mo than clone 27. Fertilization of 4-year old plantations of either clone was unwarranted, and planting clone 794 would be likely to provide greater yield than planting and fertilizing clone 27.     

牡丹江林区土壤分布规律浅析

牡丹江林区土壤分布规律为由东向西地带性土壤的垂直分布特点显著,随山体自下而上的土壤分布规律为:沼泽土→草甸土→暗棕壤→棕色针叶林土→亚高山灌丛草甸土;由西南向东北土壤的水平分布也有一定的变化趋势;因受各种成土条件及人为因素制约,不同地区土壤的小区分布也各有差异。