共查询到18条相似文献，搜索用时 62 毫秒
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华贵栉孔扇贝稚贝盐度适应性的研究 总被引：2，自引：0，他引：2
通过室内实验研究了水温28.5～29.4℃、pH值7.6～8.1条件下,华贵栉孔扇贝Chlamys nobilis(Reeve)稚贝(壳高9.77±0.19mm)对不同盐度的适应性。结果表明:华贵栉孔扇贝稚贝适宜生存盐度为24.27~37.18,最适生存盐度为26.91~32.13,适宜生长盐度为24.56~37.09,最适生长盐度为26.91~29.52。在适宜生存盐度范围内,当盐度变化超出最适范围时,低盐端变化对相对成活率、壳高日增长率、体重日增长率影响比高盐端明显。 相似文献
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墨西哥湾扇贝稚贝盐度适应性的研究 总被引：1，自引：0，他引：1
在室内控制条件下,观察不同海水盐度对墨西哥湾扇贝(Argopecten irradians concentricusSay)稚贝存活及生长的影响,并将168 h 50%死亡的盐度作为适宜生存临界盐度,将增长率为最佳增长率30%时所对应的盐度作为适宜生长临界盐度。结果表明:在稚贝壳高4.38 mm±0.31 mm,水温25.4~27.8℃,pH值7.8~8.2下,墨西哥湾扇贝稚贝适宜生存盐度为23.6~35.7,最适生存盐度为26.0~31.3;适宜生长盐度为23.9~35.8,最适生长盐度为28.7~31.3。在盐度变化超出最适范围时,`墨西哥湾扇贝稚贝对低盐更为敏感,高盐比低盐对稚贝存活、生长、增重的影响小。当盐度为28.7时,墨西哥湾扇贝稚贝具有最高的相对存活率(100%)、壳高日增长率(0.116 2 mm.d-1)及体重日增长率(1.95 mg.d-1)。当盐度在最适范围之外升高或降低,稚贝的存活率、壳高及体重日增长率也随着降低。 相似文献
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HU Guanghai ) * YAN Tong ) WANG Xiuqin ) ZHONG Delin )) First Institute of Oceanography S.O.A. Qingdao P..R.China) Ocean University of China Qingdao P..R.China 《中国海洋大学学报(英文版)》2004,3(2):195-200
1 Introduction Manhasmodifiedmanyoftheworld’scoastlines ,eitherdirectlybyconstructionordredging ,orindi rectlyasaresultofenvironmentalchangesthatinflu encesedimentsupply ,runoff,orclimate (Johns ,1995 ) .HumanactivityhasalsoproducedthemostprofoundeffectsonthecoastalenvironmentinChina .Forex ample,damconstructions ,whichrestrictpeakflowsintheupstreamoftheYellowRiver ,couldgreatlyre ducethenaturalsupplyofsedimentintotherivermouthandresultintheerosionofbeaches . Inrecentyears,manystudiescon… 相似文献
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利用山西北部应县、怀仁2个地磁台地磁Z分量观测数据,对其日变幅和低点时间进行分析。研究结果表明,2个地磁台日变幅度相近且相关性较高,日变幅年变化具有明显的季节性规律;应县、怀仁地磁台平均低点时间为北京时间12:31和12:40,低点时间相差较小,且具有夏低、春冬高的特点。 相似文献
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GUANChanglong SUNQun PhilippeFraunie 《青岛海洋大学学报(英文版)》2002,1(2):105-108
Combining the 3/2 power law proposed by Toba with the significant wave energy balance equation for wind waves, wave growth in deep water for short fetch is investigated. It is found that the variations of wave height and period with fetch have the form of power function with fractional exponents 3/8 and 1/4 respectively. Using these exponents in the power functions and through data fitting, the concise wind wave growth relations for short fetch are obtained. 相似文献
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Mt.Everest （27°54＇ N,86°54＇ E）,the highest peak,is often referred to as the earth＇s ＇third＇ pole,at an elevation of 8844.43 m. Due to the difficult logistics in the extreme high elevation regions over the Himalayas,observational meteorological data are very few on Mt. Everest. In 2005,an automatic weather station was operated at the East Rongbuk glacier Col of Mt. Everest over the Himalayas. The observational data have been compared with the reanalysis data from the National Centers for Environmental Prediction/National Center for Atmospheric Research （NCEP/NCAR）,and the reliability of NCEP/NCAR reanalysis data has been investigated in the Himalayan region,after the reanalyzed data were interpolated in the horizontal to the location of Mt. Everest and in the vertical to the height of the observed sites. The reanalysis data can capture much of the synoptic-scale variability in temperature and pressure,although the reanalysis values are systematically lower than the observation. Furthermore,most of the variability magnitude is,to some degree,underestimated. In addition,the variation extracted from the NCEP/NCAR reanalyzed pressure and temperature prominently appears one-day lead to that from the observational data,which is more important from the standpoint of improving the safety of climbers who attempt to climb Mt. Everest peak. 相似文献
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Mt. Everest is often referred to as the earth's 'third' pole. As such it is relatively inaccessible and little is known about its meteorology. In 2005, an automatic weather station was operated at North Col (28°01' 0.95" N, 86°57' 48.4" E, 6523 m a.s.l.) of Mt. Everest. Based on the observational data, this paper compares the reanalysis data from NCEP/NCAR (hereafter NCEP-Ⅰ) and NCEP-DOE AMIP-Ⅱ (NCEP-Ⅱ), in order to understand which reanalysis data are more suitable for the high Himalayas with Mt. Everest region. When comparing with those from the other levels, pressure interpolated from 500 hPa level is closer to the observation and can capture more synoptic-scale variability, which may be due to the very complex topography around Mr. Everest and the intricately complicated orographic land-atmosphere-ocean interactions. The interpolation from both NCEP-Ⅰ and NCEP-Ⅱ daily minimum temperature and daily mean pressure can capture most synoptic-scale variability (r>0.82, n=83, p<0.001). However,there is difference between NCEP-Ⅰ and NCEP-Ⅱ reanalysis data because of different model parameterization. Comparing with the observation, the magnitude of variability was underestimated by 34.1%, 28.5 % and 27.1% for NCEP-Ⅰ temperature and pressure, and NCEP-Ⅱ pressure, respectively, while overestimated by 44.5 % for NCEP-Ⅱ temperature. For weather events interpolated from the reanalyzed data, NCEP-Ⅰ and NCEP-Ⅱ show the same features that weather events interpolated from pressure appear at the same day as those from the observation, and some events occur one day ahead, while most weather events interpolated from NCEP-Ⅰ and NCEP-Ⅱ temperature happen one day ahead of those from the observation, which is much important for the study on meteorology and climate changes in the region, and is very valuable from the view of improving the safety of climbers who attempt to climb Mt. Everest. 相似文献
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In nature, Apostichopus japonicus exhibits a behavioral characteristic of emerging at night and sheltering during the day. Hence, it was commonly believed that longer and darker light conditions are better for a population of A. japonicus. In aquaculture situations therefore, animals have commonly been cultured without lighting, especially during juvenile-hatching culture. However, how the length of darkness each day affects A. japonicus and what the mechanism is of behavioral response of A. japonicus to different photoperiods remain unclear, and are specifically addressed in this study. We applied nine photoperiod treatments (light:dark (LD) cycles at 0:24, 3:21, 6:18, 9:15, 12:12, 15:9, 18:6, 21:3, and 24:0 under 500 lx) to 60 individuals (29.73 ± 0.23 g) per treatment (with 3 replicates). The environmental conditions were set as: water temperature = 16.9 ± 0.3°C, dissolved oxygen>6.0 mg/L, ammonia<0.3 mg/L, pH = 7.8-8.2, and salinity = 30-32. Under experimental conditions of continuous darkness as well as continuous light, cyclic nocturnal activity patterns of A. japonicus (viz. the animals emerged and fed at night and sheltered during the day) were observed. However, they spent more and less time, respectively, moving and feeding under continuous darkness and continuous light, than those under a natural light cycle. Under photoperiods with 6-12 h of light, the animals showed one sheltering behavior transition and two emerging behavior transitions. These behavior transitions appeared to be governed by some internal physiological factors and induced by daily light variation. The behavior of the animals was significantly affected by different photoperiods, and the distribution rate (DR) of the animals emerging at "daytime" increased with lengthening "light time" (except for the LD 3:21 cycle). We also found that there was no significant difference in mean DR per day under LD cycles of 6:18, 9:15, 15:9, and 12:12. Mean DRs per day were significantly lower for these photoperiods, than for those under LD cycles of 0:24 and 3:21, and significantly higher than for those under LD cycles of 18:6, 21:3 and 24:0. These results imply that 6-15 h light per day were the similar photoperiods to natural sunlight. From the viewpoint of activity and feeding behaviors, these might be the optimal photoperiods for rearing A. japonicus. 相似文献
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研究了云斑尖塘鳢(Oxyeleotris marmorata)幼鱼的摄食特性。结果表明:在幼鱼阶段,云斑尖塘鳢的摄食方式为主动掠食;个体全长10mm的日摄食量约为体重的11.66%,40mm的日摄食量约为体重的51.04%,69mm的日摄食量约为体重的55.30%;日摄食量与幼鱼全长呈正相关关系:A=11.3577+0.7664L(r=0.876);云斑尖塘鳢幼鱼的适口饵料鱼全长为其全长的25%～50%,幼鱼摄食15～17h后可完全消化饵料鱼;云斑尖塘鳢幼鱼昼夜摄食节律明显,一昼夜出现一个摄食高峰,高峰时段为19:00-01:00。 相似文献
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为考查具有量程扩展和原位标定功能的RZB钻孔应变仪传感器的可靠性和稳定性,设计了山洞条件下该传感器与常规传感器的定性对比实验,并对传感器日漂移量进行定量计算.通过对2019-10～2020-05观测数据进行绘图分析和计算统计,验证RZB钻孔应变仪传感器的优越性. 相似文献
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Landsat5图像的增益、偏置取值及其对行星反射率计算分析 总被引：12，自引：1，他引：11
在对比不同时相的数据或建立遥感反演模型时,往往需要将图像的灰度值转换为反射率。增益和偏置是计算反射率时使用的两个基本参数。如果这两个参数发生偏差,反射率的计算结果就有问题,大气校正和其他相关工作的结果也是不可靠的。根据USGS文档和1995年以来的Landsat5遥感图像,对图像头文件中的增益和偏置参数的取值进行了分析,并按照标准单位将增益和偏置进行了转换。为了分析不同增益和偏置取值对反射率计算结果的影响,对比计算了植被和水体的行星反射率值。对2004年7月26日的太湖地区的TM图像。取值分为4种方案: (1)使用遥感软件ENV14．0计算;(2)使用图像头文件中的参数;(3)使用USGS提供的同期参数;(4)使用USGS提供的2003年前的参数。结果表明,不同增益和偏置取值导致计算结果变化较大。如果以方案3的USGS参数计算的结果为标准,那么,其他方案的相对误差值可从0．2％到20％以上。从各个波段的误差分布看,以第3波段的相对误差最小。从工作成果的可比性角度出发,建议统一使用USGS的增益和偏置参数计算Landsat5图像的反射率。 相似文献
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