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441.
为了提高使用重力数据推断断裂构造的有效性,先以"田"字形小子域滤波法突出重力梯级带异常,再分别联合水平总梯度模、解析信号振幅及水平方向导数进行二次处理.通过理论模型试验,比较单方法及不同组合方法的处理效果,并将组合方法应用到金羊盆地实测重力数据的处理中,推断研究区的断裂构造格架.与地震剖面划分的断裂进行比对,证明了利用组合方法划分断裂构造的有效性.研究结果表明,已有断裂构造识别方法的组合应用能够更清晰地刻画地质体的边界,在应用重力数据推断断裂构造方面具有非常好的实用性.  相似文献   
442.
This study proposed a method to obtain hydrodynamic forces and coefficients for a flexible riser undergoing the vortex-induced vibration (VIV), based on the measured strains collected from the scale-model testing with the Reynolds numbers ranging from 1.34E5 to 2.35E5. The riser is approximated as a tensioned spatial beam, and an inverse method based on the FEM of spatial beam is adopted for the calculation of hydrodynamic forces in the cross flow (CF) and inline (IL) directions. The drag coefficients and vortex-induced force coefficients are obtained through the Fourier Series Theory. Finally, the hydrodynamic characteristics of a flexible riser model undergoing the VIV in a uniform flow are carefully investigated. The results indicate that the VIV amplifies the drag coefficient, and the drag coefficient does not change with time when the CF VIV is stable. Only when the VIVs in the CF and IL directions are all steady vibrations, the vortex-induced force coefficients keep as a constant with time, and under “lock-in” condition, whether the added-mass coefficient changes with time or not, the oscillation frequency of the VIV keeps unchanged. It further shows that the CF excitation coefficients at high frequency are much smaller than those at the dominant frequency, while, the IL excitation coefficients are in the same range. The axial distributions of the excitation and damping region at the dominant frequency and high frequency are approximately consistent in the CF direction, while, in the IL direction, there exists a great difference.  相似文献   
443.
Considering that the field is largely unexplored and its importance to aquaculture, outline of oomycetes and fungi parasiting on marine algae was provided in this paper, including 15 species of oomycetes, six species of chytrids, 31 Ascomycota species and one species of mitosporic fungi. In natrue, both the oomycetes and chytrids frequently occurred and induced prevalences of disease which could destroy the populations of host plants greatly. However, the parasites in Ascomycota on algae have never occurred as epidemics so far. Some issues relating to the field were discussed such as performing tests to satisfy Koch''s postulates, investigations of host specificity, interactions between host and parasite and the potential effects of environmental factors on occurrence of a disease, which are urgent in need of further investigations.  相似文献   
444.
The distributions and relationships of O_2, CO_2, and dimethylsulfide (DMS) in the Changjiang (Yangtze) Estuary and its adjacent waters were investigated in June 2014. In surface water, mean O_2 saturation level, partial pressure of CO_2 (pCO_2), and DMS concentrations (and ranges) were 110% (89%–167%), 374μatm (91–640 μatm), and 8.53 nmol L~(-1) (1.10–27.50 nmol L~(-1)), respectively. The sea-to-air fluxes (and ranges) of DMS and CO_2 were 8.24 μmol m~(-2)d~(-1) (0.26–62.77 μmol m~(-2)d~(-1)), and -4.7 mmol m~(-2)d~(-1) (-110.8-31.7 mmol m~(-2)d~(-1)), respectively. Dissolved O_2 was oversaturated, DMS concentrations were relatively high, and this region served as a sink of atmospheric CO_2. The pCO_2 was significantly and negatively correlated with the O_2 saturation level, while the DMS concentration showed different positive relationships with the O_2 saturation level in different water masses. In vertical profiles, a hypoxic zone existed below 20 m at a longitude of 123?E. The stratification of temperature and salinity caused by the Taiwan Warm Current suppressed seawater exchange between upper and lower layers, resulting in the formation of a hypoxic zone. Oxidative de-composition of organic detritus carried by the Changjiang River Diluted Water (CRDW) consumed abundant O_2 and produced additional CO_2. The DMS concentrations decreased because of low phytoplankton biomass in the hypoxic zone. Strong correlations ap-peared between the O_2 saturation level, pCO_2 and DMS concentrations in vertical profiles. Our results strongly suggested that CRDW played an important role in the distributions and relationships of O_2, CO_2, and DMS.  相似文献   
445.
The distributions and relationships of O2, CO2, and dimethylsulfide (DMS) in the Changjiang (Yangtze) Estuary and its adjacent waters were investigated in June 2014. In surface water, mean O2 saturation level, partial pressure of CO2 (pCO2), and DMS concentrations (and ranges) were 110% (89%–167%), 374 μatm (91–640 μatm), and 8.53 nmol L?1 (1.10–27.50 nmol L?1), respectively. The sea-to-air fluxes (and ranges) of DMS and CO2 were 8.24 μmol m?2 d?1 (0.26–62.77 μmol m?2 d?1), and ?4.7 mmol m?2 d?1 (?110.8-31.7 mmol m?2 d?1), respectively. Dissolved O2 was oversaturated, DMS concentrations were relatively high, and this region served as a sink of atmospheric CO2. The pCO2 was significantly and negatively correlated with the O2 saturation level, while the DMS concentration showed different positive relationships with the O2 saturation level in different water masses. In vertical profiles, a hypoxic zone existed below 20 m at a longitude of 123°E. The stratification of temperature and salinity caused by the Taiwan Warm Current suppressed seawater exchange between upper and lower layers, resulting in the formation of a hypoxic zone. Oxidative decomposition of organic detritus carried by the Changjiang River Diluted Water (CRDW) consumed abundant O2 and produced additional CO2. The DMS concentrations decreased because of low phytoplankton biomass in the hypoxic zone. Strong correlations appeared between the O2 saturation level, pCO2 and DMS concentrations in vertical profiles. Our results strongly suggested that CRDW played an important role in the distributions and relationships of O2, CO2, and DMS.  相似文献   
446.
东海泥质区表层沉积物中铜和铅的赋存形态研究   总被引:1,自引:0,他引:1  
2007年11月在东海泥质区13个站点采集了表层沉积物样品,用连续提取法分离并测定了铜和铅的赋存形态。结果表明,铜主要赋存于易还原态(铁锰氧化物结合态),含量为1.2~5.1μg/g,平均值为3.3μg/g;铅主要赋存于碳酸盐结合态,含量为1.9~7.3μg/g,平均值为5.3μg/g。泥质区铜和铅的有机结合态和易还原铁锰氧化物结合态与水深之间的呈明显的相关关系,碳酸盐结合态则与水深不相关。铜和铅非残渣态总量与采样站点水深之间的关系受控于其主要赋存形态,反映了重金属形态分布受到陆源输入和在水体中迁移等因素的影响。济州岛西南泥质区表层沉积物中铁锰氧化物结合态的铜和铅含量高于其他海区表层沉积物,可能是由于沉积物再悬浮所致。  相似文献   
447.
于2006年6月和2007年4月在长江口及毗邻海区采集了表层沉积物样品,利用水淘选法对沉积物进行了粒径分级,并采用改进后的SEDEX方法对沉积物样品及分粒级沉积物样品进行了磷形态分析。结果表明,2006年6月和2007年4月长江口及毗邻海区沉积物总磷变化分别为1256~1964 μmol/g和899~1991 μmol/g,其中碎屑磷是磷的主要存在形态。可交换态磷、铁结合态磷、有机磷、自生磷灰石磷及难分解有机磷在长江口外的平面分布比较一致,均在紧邻长江口门外、杭州湾外的条状带出现了含量的高值,而在口门内及口门外河口靠海一侧碎屑磷含量较高。不同形态磷在不同粒径沉积物中的含量不尽相同:有机磷、自生磷灰石磷以及难分解有机磷是小于8 μm粒级沉积物中磷的主要组成部分,而且其在总磷中所占比例随沉积物粒径的增加而下降;碎屑磷则主要集中在粗沉积物中,为32~63 μm及大于63 μm粒级沉积物中磷的主要贡献者。沉积物的粒度分异以及各形态磷在不同粒径沉积物中含量的差异,共同影响着河口沉积物中磷的分布  相似文献   
448.
The interspecific interactions between the rotifer Brachionus plicatilis and two harmful algal blooms (HAB) species were investigated experimentally by single culture method. B. plicatilis population and the growth of the two algae were compared at different algal cell densities. The results demonstrated that the B. plicatilis obtained sufficient nutrition from Prorocentrum donghaiense to support net population increase. With exposure to 2.5×104 cells mL−1 of P. donghaiense, the number of B. plicatilis increased faster than it did when exposed to other four algal densities (5, 10, 15 and 20 ×104 cells mL−1), and the increase rate of B. plicatilis population (r) at this algal density was 0.104 ± 0.015 rd−1. Cell densities of P. donghaiense decreased due to the grazing of B. plicatilis. In contrast, Heterosigma akashiwo had an adverse effect on B. plicatilis population and its growth was largely unaffected by rotifer grazing. In this case, B. plicatilis population decreased and H. akashiwo grew at a rate similar to that of the control.  相似文献   
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