Algae on the internet

Increasingly electronic communication and a variety of electronic resources are accessible to a larger group of people within the scientific community. This paper outlines the range of resources that are available, and comments on their current and future value to the phycological community. Resources discussed include mailing lists and newsgroups. These are useful tools for rapid, informal, targeted communication, although the technology employed places limitations on the type and format of information which may be distributed. The World Wide Web (WWW) has the potential to overcome these limitations, the quality, complexity and value to the phycological community of the sites on the WWW are extremely variable, with some material being of dubious quality. However, it is possible to access high quality resources including culture collection catalogues, high quality images and microbial and molecular databases. As well as some of the current resources, this paper discusses some possible directions for the future of phycology on the internet.http://wiua.nwi.ac.uk/     

不同施肥杨树主要营养元素内外循环比较研究 Ⅱ．施肥对落叶前后杨树叶片营养元素浓度及贮量的影响

杨树叶片在凋落前将大量有机质输入干、枝、根中,在不同处理中,不施肥输出的比例大于施肥．施Ｐ并不导致杨树对Ｐ的奢侈吸收．施肥可使杨树主要营养元素的外循环通量高于不施肥．不施肥杨树叶片在凋落前Ｐ、Ｋ的输出率比施肥高约１０％．     

水稻伸长生长的数学模型

水稻地上部诸器官的伸长生长,可以分为3个阶段和两个过渡期．器官在前期的凹型曲线生长为加速生长（定为第1阶段）,中期的直线生长为等速生长（第2阶段）,后期的凸型曲线生长为减速生长（第3阶段）;每两个阶段临界处均存在特殊的生长过程,前面的定为第1过渡期,做变加速生长,后面的定为第2过渡期,做变减速生长.组成器官的各个细胞的伸长生长,也可以分为前期凹型曲线阶段、中期的直线阶段以及这两个阶段临界处的过渡期.运用类比原理推断;细胞在凹型曲线阶段,其原生质的膨压大于壁压,而且这两个压差始终维持稳定,这就使细胞做等加速生长;细胞经过过渡期的变加速生长过渡到直线生长阶段,在这个阶段中,膨压大小与壁压相等,这就使细胞以过渡期最末的生长速度做等速生长;最后壁压大于膨压,而且这两个相差压会阻止细胞的“惯性”生长直至停止生长,其结果产生减速生长．     

棉铃虫病毒杀虫乳悬剂的生产及其药效试验

成功研制出棉铃虫病毒（ＮＰＶ）杀虫乳悬剂,改进了生产工艺和设备,建立了棉铃虫的室内品系,提高了生产效率,建立了产品的检测方法,提高了产品质量,促使棉铃虫病毒杀虫剂商品开发获得成功。大田试验证明,病毒乳悬剂的防治效果,相当于当前推广的化学农药,优于原病毒可湿性粉剂。相同剂量（０．５３一１．０７×１０（１０）ＰＩＢ／公顷）的病毒乳悬剂可使虫口平均减退９１．７％,而病毒可湿性粉剂为８３．７％。     

海河流域14种农作物对土壤库中磷的输出量和输入量初步研究

 海河流域14种农作物平均含磷量为0.127±0.053%,变化范围0.023—0.214%,不同器官中最高可达0.419%,最低仅为0.019%。对土壤库中磷输出量最大者为谷子,磷可达99.758±56.931kg·ha-1·a-1,其次是玉米和棉花;磷输入量以白薯为最大,为12.557±5.020kg·ha-1·a-1(但包括可食部分块根的输出部分在内),然后是谷子和花生,其余作物均较低,<2kg·ha-1·a-1。具高输出量的作物的部位有玉米、谷子、花生、棉花等果实,谷子、花生、白薯等茎叶;就输入量而言,除白薯为高输入和谷子为低输入类型外,其余均属很低输入型,上述特点揭示了海河流域因作物的收获而大量损失土壤库中的磷,如种植谷子、玉米、棉花等分别以99.758、32.661和26.591kg·ha-1·a-1的速率损失有效态磷。并对不同子流域作物磷的输出(入)量差异以及针对上述问题应采取的对策作了探讨。     

The biogeochemistry of a north-temperate grassland with native ungulates: Nitrogen dynamics in Yellowstone National Park

Nutrient dynamics of large grassland ecosystems possessing abundant migratory grazers are poorly understood. We examined N cycling on the northern winter range of Yellowstone National Park, home for large herds of free-roaming elk (Cervus elaphus) and bison (Bison bison). Plant and soil N, net N mineralization, and the deposition of ungulate fecal-N were measured at five sites, a ridgetop, mid-slope bench, steep slope, valley-bottom bench, and riparian area, within a watershed from May, 1991 to April, 1992.Results indicated similarities between biogeochemical properties of Yellowstone grassland and other grassland ecosystems: (1) landscape position and soil water affected nutrient dynamics, (2) annual mineralization was positively related to soil N content, and (3) the proportion of soil N mineralized during the year was negatively related to soil C/N.Grazers were a particularly important component of the N budget of this grassland. Estimated rates of N flow from ungulates to the soil ranged from 8.1 to 45.6 kg/ha/yr at the sites (average = 27.0 kg/ha/yr), approximately 4.5 times the amount of N in senescent plants. Rates of nitrogen mineralization for Yellowstone northern range grassland were higher than those measured in other temperate grassland ecosystems, possibly due to grazers promoting N cycling in Yellowstone.     

Exchange of reduced sulfur gases between lichens and the atmosphere

Fourteen lichens, 10 green algal lichens and four cyanolichens, as well as a cyanobacterium emitted significant quantities of H₂S (0.01–0.04 pmol g dw^–1 s^–1) and DMS (0.005–0.025 pmol g dw^–1 s^–1) but were sinks for COS (0.015–0.14 pmol g dw^–1 s^–1). In contrast, exchange of CH₃SH and CS₂ were sporatic and inconsistent. Although some interspecific variation occurred for the first three gases, exchange rates were relatively uniform and were not influenced by irradiance conditions. In contrast to DMS and H₂S emission, COS uptake was strongly influenced by degree of thallus hydration. Because lichen dominated systems cover extensive terrestrial habitats, COS uptake is potentially important in the world's sulfur budget.     

Fine root growth phenology,production, and turnover in a northern hardwood forest ecosystem

A large part of the nutrient flux in deciduous forests is through fine root turnover, yet this process is seldom measured. As part of a nutrient cycling study, fine root dynamics were studied for two years at Huntington Forest in the Adirondack Mountain region of New York, USA. Root growth phenology was characterized using field rhizotrons, three methods were used to estimate fine root production, two methods were used to estimate fine root mortality, and decomposition was estimated using the buried bag technique. During both 1986 and 1987, fine root elongation began in early April, peaked during July and August, and nearly ceased by mid-October. Mean fine root ( 3 mm diameter) biomass in the surface 28-cm was 2.5 t ha^–1 and necromass was 2.9 t ha^–1. Annual decomposition rates ranged from 17 to 30% beneath the litter and 27 to 52% at a depth of 10 cm. Depending on the method used for estimation, fine root production ranged from 2.0 to 2.9 t ha^–1, mortality ranged from 1.8 to 3.7 t ha^–1 yr^–1, and decomposition was 0.9 t ha^–1 yr^–1. Thus, turnover ranged from 0.8 to 1.2 yr^–1. The nutrients that cycled through fine roots annually were 4.5–6.1 kg Ca, 1.1–1.4 kg Mg, 0.3–0.4 kg K, 1.2–1.7 kg P, 20.3–27.3 kg N, and 1.8–2.4 kg S ha^–1. Fine root turnover was less important than leaf litterfall in the cycling of Ca and Mg and was similar to leaf litterfall in the amount of N, P, K and S cycled.     

The spatial variability of soil resources following long-term disturbance

The spatial distributions of selected soil properties in two adjacent sites in southwest Michigan were examined to evaluate the potential effects of chronic disturbance on resource heterogeneity. One site was a cultivated field that had been cleared, plowed, and cropped annually for decades prior to sampling while the other, uncultivated field was cleared of original forest in 1960 after which it was mown annually but never plowed or cropped. We took replicate samples from a 330-point unaligned grid across the sites for soil pH, gravimetric moisture, inorganic phosphorus, total carbon, and net nitrification and nitrogen mineralization potentials. Soils in the cultivated site contained less than half as much carbon as in the uncultivated site, but had higher levels of inorganic phosphorus and moisture, and higher soil pH. Potential net nitrogen mineralization and nitrification rates did not differ between sites. Geostatistical analysis showed that almost all properties examined were strongly autocorelated within each site; structural variance as a proportion of sample variance ranged from 30–95% for all properties, and for any given property differed little between sites. The distance over which this dependence was expressed, however, was for all properties but pH substantially less in the uncultivated site (7–26 m) as compared to the tilled site (48–108m), especially for total C and net nitrification and N mineralization. These results suggest that the spatial pattern and scale of soil variability can differ markedly among edaphically identical sites and that these differences can be related to disturbance history.