Profile of Methane Concentrations in Soil and Atmosphere in Alpine Steppe Ecosystem on Tibetan Plateau

The methane concentration profile from -1.5m depth in soil to 32m height in air was measured in alpine steppe located in the permafrost area. Methane concentrations showed widely variations both in air and in soil during the study period. The mean concentrations in atmosphere were all higher than those in soil, and the highest methane concentration was found in air at the height of 16m with the lowest concentration occurring at the depth of 1.5m in soil. The variations of atmospheric methane concentrations did not show any clear pattern both temporally and spatially, although they exhibited a more steadystable state than those in soil. During the seasonal variations, the methane concentrations at different depths in soil were significantly correlated （R^2〉0.6） with each other comparing to the weak correlations （R^2〈0.2） between the atmospheric concentra- tions at different heights. Mean methane concentrations in soil significantly decreased with depth. This was the compositive influence of the decreasing production rates and the increasing methane oxidation rates, which was caused by the descent soil moisture with depth. Although the methane concentrations at all depths varied widely during the growing season, they showed very distinct temporal variations in the non-growing season. It was indicated from the literatures that methane oxidation rates were positively correlated with soil temperature. The higher methane concentrations in soil during the winter were determined by the lower methane oxidation rates with decreasing soil temperatures, whereas methane production rates had no reaction to the lower temperature. Relations between methane contribution and other environmental factors were not discussed in this paper for lacking of data, which impulse us to carry out further and more detailed studies in this unique area.     

利用城市污泥堆肥及建筑弃土种植麦冬研究

将污泥堆肥产品分别与建筑弃土按0%、10%、20%、30%、40%和50%(湿重)的比例配制营养土,以麦冬为例进行180 d的栽培实验,分析了营养土对麦冬生长特性、植物体内及栽培土壤中营养学指标和重金属含量的变化规律,并通过模糊综合评价方法选择营养土较佳配制方案。实验结果表明:堆肥比例在50%时麦冬生物量增加率、新生芽数及地表部分比重为最大值,在30%时纺锤体肉质数减少率为最大值;随着营养土中堆肥比例增加,麦冬体内养分含量、重金属积累量随之增加,均在50%时达到最大值;栽培土壤养分越多损失量越多,各指残留率越低,同时全磷、全氮及K含量降低率较有效磷、碱解氮小得多,Cr降低率在5.20%～8.34%之间,Zn降低率在3.27%～17.35%之间;堆肥比例在40%以上的营养土对麦冬生长效果好,但较佳配制方案为堆肥产品占20%。     

嘉陵江吻(鱼句)生长和繁殖力研究

本文根据采自嘉陵江合川江段的483尾标本,研究吻(鱼句)的生长和繁殖力,并对其资源的增殖保护和合理利用提出初步意见。     

郫县灰潮田有效硅含量和小麦施硅效应初探

通过同田对比试验，本文对郫县水稻土小麦施用硅肥进行了初步研究．结果表明，小麦施硅获得了增产效果；施硅对小麦穗粒数、株高和基部节间体积等具有生长效应；郫县水稻土有效硅含量为１２７±３９ｍｇ·ｋｇ－１（ｎ＝１２），变异较大，与土壤粘粒（＜０．００１ｍｍ）呈极显著正相关（ｒ＝０．７９）；发育于第四系岷江灰色冲积母质的郫县水稻上，粘粘含量普遍较低，因此，郫县小麦施硅具有较大增产潜力．     

滨海平原咸水入侵动态监测网构建研究——以潍河下游地区为例

作为进行咸水入侵动态监测的基础性工作，对潍河下游地区的供需水平衡及地下水位、水质和地层电阻率在咸淡水界面上变化规律进行了研究分析；同时，探索了监测工作的地理工程技术途径，并据此构建了3个层次的监测体系：（1）宏观区域供需水平衡分析与地下水位负值区变化监测，（2）中观咸水入侵发展变化的物探监测，（3）微观地下水位、水质变化监测；最后，为了对日益增多的咸水入侵动态数据资料进行有效的管理，设计了一个基于GIS的、以数据库管理应用为核心的信息系统。     

我国煤系地层高岭岩综合利用的问题与对策

本文简述了我国煤系地层高岭岩的分布、储量及重要性等,指出了综合利用的基本方向,对目前存在的问题进行了讨论,提出了对策。     

超补偿理论及其在虫害控制中的意义

本文较为系统地阐述了作物对虫害损伤的超补偿理论,表明超补偿广泛存在于各种作物中,并对超补偿所需条件、基本原因以及与害虫控制的关系作进一步讨论。     

降解苯酚优势菌的筛选分离和培养条件研究

从膨润土中筛选出可在含2 g/L苯酚的PDA培养基上生长的菌种,经过逐级驯化,得到1株可以在1 g/L苯酚的无机盐固体培养基上生长并降解苯酚的优势菌种HJ01,其对苯酚600 g/L降解率可达94%.该菌生长的适宜碳源和氮源分别为蔗糖和NH4Cl,温度为25 ℃,pH值范围为6-7.     

睫毛萼凤仙花响应土壤水分和竞争的表型可塑性

研究了睫毛萼凤仙花在干、湿两种土壤水分条件下和密、疏两种栽种密度条件下形态和生长的表型可塑性。睫毛萼凤仙花在土壤水分饱和条件下的形态参数和生物量积累都高于干旱条件,在稀疏栽植下的形态参数和生物量积累也高于密集栽种。睫毛萼凤仙花通过调整器官生物量分配和形态参数来适应不利的环境,但付出了减少后代数目的代价。睫毛萼凤仙花适宜在土壤水分充足、植株密度不高的生境中生长。