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111.
Maximum Entropy Spectral Analysis and Multiple Regression Analysis of the 200 year series (1781–1980) of the change in L.O.D. (Length of Day) revealed significant peaks atT=21, 32, 50, 63 and possibly 120 years. The periodsT=22 and 44 years seem to be stable over 200 years.  相似文献   
112.
Vast declines in Zostera marina seagrass beds demand effective methods of rehabilitation. In this study, we developed a practical method by reducing salinity to induce seed germination followed with recovering salinity to facilitate seedling production of Z. marina. The results showed that Z. marina seeds collected from natural seawater(salinity 30) were induced to germinate at reduced salinities. Percent germination(GR) was higher and mean-time-to-germinate(MTG) was shorter at lower salinities. The highest GR and shortest MTG occurred at salinity 0(deionized freshwater). After germination in freshwater, seeds could develop into seedlings at salinities5–30 and continue the growth. Viability or development of germinated seeds was not significantly different during the 40 d of post-germination incubation at salinities 5–15 after 1–20 d of germination in freshwater. However,during the process of translating germinated seeds from salinity 0 and 5 to salinity 30, reducing the gradients of post-germination acclimation facilitated more seeds forming seedlings in less time. On average, after 60 d of static incubation, including 20 d in freshwater for germination followed with immediate shift to salinity 5 and increasing to salinity 30 at increment of 5 every two days until cultivation at constant salinity 30, 33% of Z. marina seeds produced healthy seedlings. The results indicate that the salinity-manipulation based method of artificial germination and seedling production is practical and effective in supporting rehabilitation of Z. marina bed.  相似文献   
113.
浑善达克沙地沙丘剖面颜色变化的古气候意义   总被引:2,自引:0,他引:2  
为研究中国沙漠东部广泛分布的风成沙-古土壤沉积序列的颜色变化与古气候之间的可能联系,以浑善达克沙地为研究区,测定了7个天然风成沙-古土壤沉积序列的颜色(L*a* b*)、有机碳、总氮和粒度。结果表明:L*(亮度)、a*(红度)、b*(黄度)值分别介于32.41~65.89,2.73~7.52和-1.68~17.16;L*、a*、b*值之间存在正相关关系,其中L*和b*之间的相关性最显著(R2=0.90),而L*和a*之间的相关性最低(R2=0.26);L*、a*、b*值在垂直方向上具有相同的变化趋势和特征,它们在风成沙层位处为高值,在灰色-黑色砂质古土壤层位处为低值,但L*值变化较大,a*和b*值变化较小。均值的非参数检验表明L*可指示风成沙-古土壤沉积序列的风成沙和古土壤层的变化,而a*在这类沉积序列上变化不敏感。影响L*的主要因素与有机质含量和成壤作用有关,它们都与东亚夏季风强弱变化关系密切,因此L*有明确的古气候意义;L*低值对有机质含量增加和成壤作用的加强具有指示作用,是东亚夏季风增强的信号。基于颜色参数L*可以很好地重建中国沙漠东部风成沙-古土壤沉积序列的古气候变化。  相似文献   
114.
In the margin of southern Junggar basin, there is a potential of shale gas with the upper Permian l.uoaogou Formation. For a detailed understanding and evaluation with the shale gas geological characteristics of l.uoaogou Formation, the petrologic characteristics of the carbonaceous shale was researched, and the results show that: ( 1 ) in l.ucaogou Formation, the mean value of the brittle mineral percentages of the upper member, the middle member and the lower member are all more than 50%, but it is the highest in the middle member, and it is second in the lower member. At the same time, in the lower member, the mean value of the brittle mineral percentages is significantly lower than the upper and middle members; (2)the main brittle mineral in each member are quartz+feldspar, and there is a same change rule between the quartz+feldspar content and the total brittle mineral, that is; The quartz + feldspar content is the highest in the middle member, followed with the lower member, and it is obviously low in the upper member; (3 )from the lower member to the upper member, the content of carbonate in the carbonaceous shale are gradually reduced; (4) the clay mineral content of the carbonaceous shale of the upper member is far higher than the lower and middle members. And the clay mineral in each member are mainly constituted with illite and illite/Mongolia inter layer; ( 5 ) in the northern margin of the western part of the Bogda Mountain, south Junggar Basin, the brittle mineral content of the carbonaceous shale generally present as a decreasing trend from west to east to Fu Rang.  相似文献   
115.
116.
使用透射电镜和萤光抗体染色,对处于可培养和活的非可培养状态的霍乱弧菌进行了细胞形态结构比较研究。结果表明:处于非可培养状态的霍乱菌细胞,体积明显地缩小,形态由弧形变成了球形,我们共观察了382个非可培养状态的细胞,发现它们的细胞壁都是完整的,即不是细菌-L型,在这些细胞中也都没发现芽孢结构  相似文献   
117.
泥蚶及菲律宾蛤仔对环境中氨的耐受力   总被引:1,自引:0,他引:1  
汪心沅 《海洋科学》1989,13(6):51-54
本文对泥蚶成贝、幼贝,菲律宾蛤仔成贝、幼贝的未离解氨氮 168h LCD_(50),EC_(50)(降低耐低氧环境能力50%的浓度)进行了试验,并对氨的致死和亚致死浓度与内湾养虾水域(乳山东湾)、试验虾池及利用虾池水的试验贝池底质环境的氨氮水平作了概略评价。  相似文献   
118.
微波辐射计遥感海水盐度的水池实验研究   总被引:1,自引:0,他引:1  
通过水池实验研究了L波段微波辐射和盐度的关系,并进行了盐度的反演计算。实验中,先向水池内加入天然海水,然后通过向水池中添加自来水的方式调节降低池内水体的盐度,使盐度从31.67逐步降低到27.48。在此期间,利用微波辐射计观测池内水体的L波段H极化和V极化辐射值以及S波段V极化辐射值,利用CTD观测池内水体的温度和盐度。L波段微波辐射值和根据辐射理论计算出的亮温值具有很好的线性关系。利用最大和最小的2个盐度下的微波辐射值和由辐射理论计算的亮温得到定标公式,将观测的辐射值换算为亮温。最后利用半解析的反演算法反演盐度。本次实验的反演最大误差为2.1,均方差为0.3。  相似文献   
119.
Abstract. Combined effects of temperature, salinity, and metal enrichment (Zn, Mn, Co) on the growth rate and chemical composition of Fucus vesiculosus L. were studied in culture. Factorial combinations of two temperatures and three salinities were used. The results indicated that the accumulation of Zn and Mn into algal tissue was enhanced by dilution of the media, whereas Co accumulation exhibited maxima at the medium salinity. Zn accumulation was enhanced by temperature, while the opposite was true for Mn and Co.
In the presence of metals the usual dilution-induced changes in growth activity and chemical composition of Fucus plants were altered, while responses to the temperature factor remained unchanged. In diluted media, growth activity and mannitol content decreased along with a simultaneous increase of protein content. In the presence of Zn and Mn the mannitol content exhibited peaks at the medium salinity; in the presence of Co the dilution-induced pattern remained unchanged. Salinity-induced changes in growth and protein content were altered in the presence of metals. Maxima in growth rates were found at the medium salinity. Growth was higher in extremely diluted media than in scawater, indicating an inversion of responses to the salinity factor. Both the growth rate and mannitol content were lowest under the influence of Zn.  相似文献   
120.
大菱鲆产卵季节对卵子的生物学及生化特征的影响   总被引:13,自引:10,他引:13  
于2000年6-8月,采用现场测定和生化分析方法,研究了大菱Ping雌鱼产卵盛期和产卵晚期卵子的生物学特征及生化组成。结果表明,大菱Ping卵子的生物学特征及生化组成随着产卵季节的进程而改变。产卵晚期的卵子卵径小于产卵盛期,每粒卵子含水量及重量均高于晚期,盛期卵子的粗蛋白、脂肪、灰分占干重的百分比低于晚期卵子。在产卵晚期,中性脂所产卵盛期有明显增加,而20:5(n-3)、20:4(n-6)水平比产卵盛期有明显增加,而20:5(n-3)、20:4(n-6)、22:5(n-3)和22:6(n-3)的水平则明显下降。产卵盛期卵子的孵化率和存活力要高于晚期。  相似文献   
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