浙江天童植物群落演替对土壤化学性质的影响

对浙江天童植物群落演替过程的土壤腐殖质层、0～10cm层和10～20cm层化学因子的比较研究结果表明,随着进展演替,土壤全氮含量呈明显增长趋势,但硝态氮、氨态氮、速效氮、速效磷和速效钾含量除演替初期的裸地、灌丛较小外,森林群落阶段增长趋势一般不明显;土壤pH值则缺乏明显的规律性,但有机质含量呈明显增长趋势,而富里酸和胡敏酸含量,除栲树木荷林和栲树林较高,裸地最低外,其它演替阶段增长趋势也不明显;HA/FA在腐殖质层缺乏明显的规律性,但在0～10cm和10～20cm层则呈减少趋势。可见,常绿阔叶林次生演替能增加土壤有机物质含量,促进土壤有机物质的矿化和再合成作用;而土壤化学性状的改善,也为常绿阔叶林的进展演替奠定了基础。     

岷江上游干旱河谷植被恢复环境优化调控技术研究

针对岷江上游植被恢复困难地段的主要限制因子,进行了３ 年的调控试验及其定位观测研究．结果表明,大面积栽植的土壤环境优化调控技术措施是：头年雨季前水平沟整地,挖中等大小的植坑,同时点播绿肥沙打旺,第２ 年雨季施磷肥植苗;或头年雨季前水平沟整地,挖中等大小的植坑,第２ 年雨季施磷肥植苗同时用石块覆盖．该技术措施简单易行,已在该区推广应用     

北京地区植被景观中斑块大小的分布特征

利用GIS软件ARC／INFO将北京地区的1：20万植被图数字化,并提取各斑块的面积信息。该图包含72个基本的斑块类型,它们又分属于森林、灌丛、草地、果园、农田和水体6大类型。这些大类又分别包含20、28、4、7、11和2个基本类型。选用斑块个数、总面积、平均斑块面积、标准差、变异系数、中值、最大斑块面积、最小斑块面积、极差和偏态系数等几个描述统计量,以及厂一分布、对数正态分布、Weibull分布、指数分布和正态分布等5个概率分布来刻画斑块大小的分布特征。结果表明：除具有很少斑块的少数基本类型以外,其它基本类型以及所有6个大类的斑块大小的分布都不是对称的,而是右偏的。因此,普通的正态分布不能对它们加以刻画;其他4种概率分布也只能刻画部分类型,并且服从对数正态分布的类型最多,服从负指数分布的斑块类型最少。     

末次冰盛期低海面时南海南北陆架上的植被

在探讨孢粉的传播、来源地的基础上,根据南海南北陆坡柱状剖面（１７９４０ ,１７９６４） 的孢粉资料推断末次冰盛期（包括氧同位素３ 期的上部） 低海面时,南北出露的大陆架上生长的植被。末次冰盛期时北部大陆架曾分布以蒿属（Ａｒｔｅｍｉｓｉａ Ｌ．） 为主的草原植被,气候较今日冷且干旱。南部称为“巽他古陆”,曾覆盖热带低地雨林,河口及海岸为红树林,在周围岛屿上高山雨林曾多次向山下迁移,表明当时温度可能较今日低,但湿度没有明显变化。南北大陆架末次冰期时在植被与气候演化上的巨大差异,可能与南部巽他陆架的特殊位置（ 西太平洋暖池） 有关     

Persistence of Toxic Activity and Recycling of Bacillus thuringiensis var. israelensis in Cold Water: Field Experiments Using Diffusion Chambers in a Pond

The persistence of the larvicidal activity of Bacillus thuringiensis var. israelensis (Bti) was tested over a five-month period in a low-temperature aquatic environment. Diffusion chambers filled with a suspension of Bti (100 mg l - 1) and different experimental substrates (pond water, periphyton, sediments and vegetation), but without mosquito larvae, were placed near the bottom of a large pond and removed at various intervals to measure residual toxic activity to mosquito larvae, spore concentration and proteolytic activity. Within the pond water substrate, 50% of the initial toxicity was still present after one month in cold water, while with the periphyton substrate, 30% remained in the liquid fraction after the same period of exposure. Within the vegetation substrate (blue-joint grass, Calamagrostis canadensis), an average of 30% of the initial toxicity was still present in the liquid fraction between day 84 to day 154. Solid fractions of vegetation became toxic very early and remained toxic for five months. At the end (day 154), there was still 54% of the original toxic activity put in the chambers associated with the vegetation samples. In the absence of mosquito larvae, spore recycling was observed in the chambers especially with sediments and vegetation. But spore recycling did not appear to play a major role in the observed persistence, but rather rapid absorption onto vegetation substrates was responsible for the persistence of Bti in a cold climate.     

粘型小麦不育系育性恢复性的细胞遗传学研究

利用5个粘性不育系分别与中国春的二体,1B重双端体及1B°1D^Ⅳ缺四体杂交,调查其F1的育性及其F1减数分裂中期Ⅰ的染色体配对情况和后期Ⅰ出现落后染色体的细胞频率。结果表明：（1）5个不育系与中国春二体杂交F1的自交结实率存在明显差异。中国春的1B重双端体使5个不育系的自交结实率大幅度下降,中国春的1B°1DⅣ缺四体使各不育系表现全不育;（2）5个不育系和3个父本杂交F1减数分裂中期Ⅰ出现单价体细胞的频率与其后期Ⅰ出现落后染色体细胞的频率不存在直接相关;（3）5个不育系与中国春二体的杂交F1自交结实率与其减数分裂中期Ⅰ出现单价体细胞的频率呈正相关。相关系数为0.9695**,与后期Ⅰ出现落后染色体细胞的频率不直接相关。     

Stream power influence on southern Californian riparian vegetation

Abstract. Mechanical damage by floodwaters is frequently invoked to explain the distribution of riparian plant species, but data have been lacking to relate vegetation to specific estimates of flood damage potential. This research uses detailed estimates of unit stream power (an appropriate measure of the potential for mechanical damage) in conjunction with vegetation cover data to test this relationship at 37 valley-bottom sites in the Transverse Ranges of Southern California. A computer program, HEC-2, was used to model the slope and the variation in flow depth and velocity of the 20-yr flood across the sites. Regression models tested the influence of stream power (and of height above the water table) on the woody species composition of 393 4-m cross-section segments of the valley-bottom sites. Results indicate that unit stream power does have a significant effect on the riparian vegetation, but that the amount of that influence and its importance relative to the influence of height above the water table varies between watersheds. Some species are found primarily in locations of high stream power, while others are limited to portions of the valley bottom that experience only low stream power.     

Interannual Variability in Terrestrial Net Primary Production: Exploration of Trends and Controls on Regional to Global Scales

Climate and biophysical regulation of terrestrial plant production and interannual responses to anomalous events were investigated using the NASA Ames model version of CASA (Carnegie–Ames–Stanford Approach) in a transient simulation mode. This ecosystem model has been calibrated for simulations driven by satellite vegetation index data from the National Oceanic and Atmospheric Administration (NOAA) Advanced Very High Resolution Radiometer (AVHRR) over the mid-1980s. Relatively large net source fluxes of carbon were estimated from terrestrial vegetation about 6 months to 1 year following El Niño events of 1983 and 1987, whereas the years 1984 and 1988 showed a drop in net primary production (NPP) of 1–2 Pg (10¹⁵ g) C from their respective previous years. Zonal discrimination of model results implies that the northern hemisphere low latitudes could account for almost the entire 2 Pg C decrease in global terrestrial NPP predicted from 1983 to 1984. Model estimates further suggest that from 1985 to 1988, the northern middle-latitude zone (between 30° and 60°N) was the principal region driving progressive increases in NPP, mainly by an expanded growing season moving toward the zonal latitude extremes. Comparative regional analysis of model controls on NPP reveals that although Normalized Difference Vegetation Index “greenness” can alone account for 30%–90% of the variation in NPP interannual anomalies, temperature or radiation loading can have a fairly significant 1-year lag effect on annual NPP at middle- to high-latitude zones, whereas rainfall amount and temperature drying effects may carry over with at least a 2-year lag time to influence NPP in semiarid tropical zones.     

蒙古栎红松林演替模型FOROAK的研究

Based on forest dynamics theory, gap model FOROAK was developed for simulating long-termdynamics of Mongolian oak (Quercus rnongolica Fisch. )-Korean pine (Pinus koraiensis Sieb. et Zucc. )forest. The model included two parts: biological growth and environmental impacts on growth. Different areapatches were used in simulating forest changes. The results showed that this forest gap was 0.05 hm2. Themodel testing demonstrated that it could reasonably simulate forest dynamic process, and had a very highaccuracy to predict species compositions. The observed species basal areas was similar to the predicted at 60,100 and 270 year forests, the observed species compositions were similar to the predicted at old forest period.Complex changes were found through modeling forest dynamics of bare ground. Mongolian oak and white birch( Betula platyphylla Sukacz. ) dominated at early stage, forest dominated by broad leaved species was formedat middle stage, and then Korean pine dominated at latter stage. The prediction of current primary forestshowed that it was steady during the next 300 year period, the number of trees and the biomass of Korean pine changed very little.     

An Insight into Paleovegetation on the Emerged Shelf at the Last Glaciation: Pollen Date of the South China Sea

Vegetation on the emerged continental shelves of the South China Sea (SCS) during the Last Glacial Maximum (LGM) was deduced based on pollen of hemipelagic sediments from the continental slopes and the consideration of pollen transport dynamics and source areas. During the LGM (including the top of Oxygen Isotope Stage 3) the sea level might be more than 100 m lower than that of the present. Consequently, both northern and southern continental shelves of the SCS were exposed. The northern continental shelf was covered by grassland mainly of Artem/s/a. The climate should be cold and dry, whereas on the southern continental shelf (Sunda Land) was spread tropical lowland rainforest and mangroves were scattered by the river mouths and along the coast. The climate might be cooler than that in the present day, but drop of humidity was not observed.