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131.
Analysis and comparison of Jiaozhou Bay data collected from May 1991 to February 1994 (12 seasonal investigations) provided
by the Ecological Station of Jiaozhou Bay revealed the characteristic spatiotemporal variation of the ambient concentration
Si∶DIN and Si∶16P ratios and the seasonal variation of Jiaozhou Bay Si∶DIN and Si∶16P ratios showing that the Si∶DIN ratios
were <1 throughout the year in Jiaozhou Bay; and that the Si∶16P ratios were <1 throughout Jiaozhou Bay in spring, autumn
and winter. The results proved that silicate limited phytoplankton growth in spring, autumn and winter in Jiaozhou Bay. Analysis
of the Si∶DIN and Si∶P ratios showed that the nutrient Si has been limiting the growth of phytoplankton throughout the year
in some Jiaozhou Bay waters; and that the silicate deficiency changed the phytoplankton assemblage structure.
Analysis of discontinuous 1962 to 1998 nutrient data showed that there was no N or P limitation of phytoplankton growth in
that period. The authors consider that the annual cyclic change of silicate limits phytoplankton growth in spring, autumn
and winter every year in Jiaozhou Bay; and that in many Jiaozhou Bay waters where the phytoplankton as the predominant species
need a great amount of silicate, analysis of the nutrients N or P limitation of phytoplankton growth relying only on the N
and P nutrients and DIN∶P ratio could yield inaccurate conclusions. The results obtained by applying the rules of absolute
and relative limitation fully support this view.
The authors consider that the main function of nutrient silicon is to regulate and control the mechanism of the phytoplankton
growth process in the ecological system in estuaries, bays and the sea.
The authors consider that according to the evolution theory of Darwin, continuous environmental pressure gradually changes
the phytoplankton assemblage's structure and the physiology of diatoms. Diatoms requiring a great deal of silicon either constantly
decrease or reduce their requirement for silicon. This will cause a series of huge changes in the ecosystem so that the whole
ecosystem requires continuous renewal, change and balancing. Human beings have to reduce marine pollution and enhance the
capacity of continental sources to transport silicon to sustain the continuity and stability in the marine ecosystem.
This study was funded by the NSFC (No. 40036010) and subsidized by Special Funds from the National Key Basic Research Program
of P. R. China (G199990437), the Postdoctoral Foundation of Ocean University of Qingdao, the Director's Foundation of the
Beihai Monitoring Center of the State Oceanic Administration and the Foundation of Shanghai Fisheries University. 相似文献
132.
中国西部植被水分利用效率的时空特征分析 总被引:8,自引:1,他引:8
利用净初级生产力模型C-FIX,陆面过程模型CoLM以及高时空分辨率的遥感数据集,定量估算了2002年西部地区1 km分辨率的水分利用效率(WUE)时空格局分布.模型估算2002年西部地区净初级生产力总量约为0.96 PgC,蒸散发总量约为2 098 km3,整个西部地区平均单位面积上年均WUE约为0.32 gC.mm-1.西部地区WUE时空分布格局具有显著的异质性:WUE最高值区主要分布在新疆西北部的天山和阿尔泰山区域,年均WUE最高可达4 gC.mm-1.m-2;其次为西藏东南隅以及陕西和甘肃南部山区,年均WUE约在1~2 gC.mm-1.m-2之间.WUE最低值广泛分布在青藏高原地区和西北沙漠地区,年均WUE基本在0.4 gC.mm-1.m-2以下.研究发现,西北干旱区内陆河流域荒漠植被呈现出相对高的WUE水平,反映出适度水分亏缺地区的天然植被生态系统可能具有较水分充足地区植被生态系统更高的水分利用效率功能.通过定量分析比较不同植被生态系统WUE特征及其季节变化廓线,得到西部地区主要植被生态系统的年均WUE大小为山区森林>荒漠乔灌丛>灌溉农田>高寒草地>寒漠和戈壁. 相似文献
133.
134.
1971—2000年中国陆地植被净初级生产力的模拟 总被引:4,自引:0,他引:4
利用植被与大气相互作用模式(AVIM),基于气象台站的观测资料模拟了1971—2000年中国陆地生态系统NPP的变化特征.结果表明:1971—2000年我国陆地植被年均NPP变化范围在0~987.67 gC·m-2·a-1,全国平均值为349.74 gC·m-2·a-1,30 a呈现出递增的变化趋势.对各类植被NPP的模拟显示,最近30 a我国热带雨林、落叶阔叶林以及有地被层的阔叶林的年均NPP减小,而混交林、常绿针叶林、落叶针叶林、有裸土的灌丛、草地以及作物的年均NPP均为增加趋势.由于采用了先进的农业技术,与自然条件下我国作物的年均NPP变化相比,我国实际的粮食单产在上述时期呈显著的增长,表明了人类活动对于我国陆地植被净初级生产力有着深刻的影响. 相似文献
135.
我国海洋初级生产力研究二十年 总被引:14,自引:1,他引:13
回顾和论述了我国学者近 2 0年来在海洋初级生产力观测研究的进展。随着我国资源与环境问题的日益突出 ,初级生产力研究越来越受到重视 ,研究海域也越来越广阔 ,研究的方法不断改进与完善。 2 0年来我国海洋初级生产力研究取得了很大成绩 ,基本搞清了我国海域的状况 ,为生态系结构与功能研究、为渔业资源的合理开发与可持续发展、为海洋环境质量的评价和赤潮的监测与预报等提供了重要科学基础。目前该项研究正在向更广和更深的层次发展 ,并且与特定的研究目标紧密联系 ,有些研究项目已与国际接轨。加强大空间尺度和长时间序列的观测研究及其与相关学科的综合研究 ,和采用现代化的观测手段 ,必将使该领域的研究提到一个更高的水平。 相似文献
136.
东海异养细菌生产力的时空分布 总被引:11,自引:2,他引:9
1997年 2— 3月和 1 998年 7月 ,在东海海区乘“科学一号”考察船进行两个航次的调查 ,利用异养细菌特异示踪物 [甲基 - 3H]胸腺嘧啶核苷 (3H -Tdr)并入DNA的速率测定东海 (2 7°— 32°N ,1 2 2°— 1 30°E)异养细菌生产力 (BP)。结果表明 ,1 997年 2— 3月 (冬季 )异养细菌生产力较低 [0 46— 2 62 μgC/(L·h) ],1 998年 7月 (夏季 )异养细菌生产力较高 [3 50—1 5 70 μgC/(L·h) ]。冬季和夏季在长江口和 41 0站附近都有一个异养细菌生产力的高值区。通过两个连续站的昼夜观测发现冬季异养细菌生产力变化是底层 >中层 >表层 ,夏季是中层>底层 >表层。异养细菌生产力与初级生产力 (PP)之比 ,即BP PP ,冬季的均值为 0 1 7(0 0 4— 0 30 ) ,夏季的均值为 0 32 (0 2 1— 0 43)。BP PP冬季的高值区在长江口附近 ,夏季的高值区在 1 1 1站附近 ,这与长江冲淡水有密切相关。 相似文献
137.
东海初级生产力遥感反演及其时空演化机制 总被引:1,自引:0,他引:1
According to calculation results of ocean chlorophyll concentration based on SeaWiFS data by SeaBAM model and synchronous ship-measured data, this research set up an improved model for Case I and Case Ⅱ water bodies respectively. The monthly chlorophyll distribution in the East China Sea in 1998 was obtained from this improved model on calculation results of SeaBAM. The euphotic depth distribution in 1998 in the East China Sea is calculated by using remote sensing data of K490 from SeaWiFS according to the relation between the euphotic depth and the oceanic diffuse attenuation coefficient. With data of ocean chlorophyll concentration, euphotic depth, ocean surface photosynthetic available radiation (PAR), daily photoperiod and optimal rate of daily carbon fixation within a water column, the monthly and annual primary productivity spatio-temporal distributions in the East China Sea in 1998 were obtained based on VGPM model. Based on analysis of those distributions, the conclusion can be drawn that there is a clear bimodality character of primary productivity in the monthly distribution in the East China Sea. In detail, the monthly distribution of primary productivity stays the lowest level in winter and rises rapidly to the peak in spring. It gets down a little in summer, and gets up a little in autumn. The daily average of primary productivity in the whole East China Sea is 560.03 mg/m^2/d, which is far higher than the average of subtropical ocean areas. The annual average of primary productivity is 236.95 g/m^2/a. The research on the seasonal variety mechanism of primary productivity shows that several factors that affect the spatio-temporal distribution may include the chlorophyll concentration distribution, temperature condition, the Yangtze River diluted water variety, the euphotic depth, ocean current variety, etc. But the main influencing factors may be different in each local sea area. 相似文献
138.
土地利用和气候变化对区域净初级生产力影响 总被引:4,自引:2,他引:2
1IntroductionThe global change caused by the continuous increasing concentration of atmospheric greenhouse gases has threatened the existence of human beings, and the importance of carbon dioxide emissions as a major environmental issue of international concern has grown substantially in the world (IPCC, 2000). At the same time, the Kyoto Protocol, the first and only realistic plan for achieving a worldwide reduction in greenhouse gas emissions, has been passed. Since there are many uncertai… 相似文献
139.
140.
本文以MOD17A3HGF植被净初级生产力(NPP)数据为基础,结合气温、降水及DEM数据,开展了2000—2020年黄河流域植被NPP时空变化特征及其对水热条件和退耕还林还草工程实施的响应研究。结果表明:(1)黄河流域植被NPP总体呈显著线性增加趋势(P<0.001),其中植被NPP增速中游地区高于下游、下游高于上游地区。黄河流域植被NPP显著增加趋势占95.29%,集中分布在黄河流域中游地区(黄土高原地区);显著减少的区域主要集中在人口分布密集的城市及其周边区域。(2)黄河流域植被NPP与年平均气温、年降水量均以正相关为主,其中显著正相关分别占11.15%和42.35%,分别呈东—西向和南—北向分布。(3)黄河流域中游地区坡度为[15°,25°]区域植被NPP增速最快,其次为坡度>25°和<15°区域,反映出退耕还林还草工程的实施对黄河流域中部黄土高原地区的植被改善具有一定的作用。 相似文献