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1.
万能  孙科  范伟国  田欢  严森  谢淑云  向武  鲍征宇 《地球科学》2020,45(3):1041-1050
江汉平原是中国四大粮仓之一,拥有约69万公顷富硒土壤,大部分为冷浸田,如何利用富硒冷浸田种植富硒水稻是当前亟需研究解决的重大实际问题.以排水整改、强化施硒肥和排水整改后施硒肥3种模式开展了江汉平原富硒冷浸田的大田种植实验.结果表明,在排水整改模式下,排水降低了冷浸田地下水位,提升了土壤的通气性和氧化还原电位,加快了土壤中有机结合态硒向可利用态硒转化,使得土壤可利用态硒比整改前提高25.0%;促进了水稻对硒的吸收,使得水稻根系和籽实中硒含量比整改前分别增加20.6%和8.3%,仅茎干中硒含量无明显变化.在强化施硒肥模式下,每亩施加80 kg硒肥后土壤可利用态硒比施肥前提高41.7%;极大地促进了水稻对硒的吸收,使得水稻根系、茎秆、籽实中硒含量比施肥前分别提升79.4%、37.1%、25.0%.在冷浸田排水整改后每亩施加80 kg硒肥模式下,土壤可利用态硒含量和水稻根系、茎干、籽实中硒含量分别增加50.0%和41.8%、46.1%、47.9%.总之,上述3种利用模式均可提高土壤可利用态硒含量,有利于水稻对土壤硒的吸收,能够显著提高水稻籽实中硒含量;冷浸田排水整改后强化施硒肥利用模式效果最佳.   相似文献   
2.
In the East China Sea(ECS), the succession of causative species responsible for blooms is a recurrent phenomenon during the spring, which changes from diatoms to dinoflagellates. Observations from space and in situ cruises captured this pattern of succession during spring of 2005. In this study, we coupled two biological models, which were developed previously for Skeletonema costatum and Prorocentrum donghaiense,into a circulation model tailored for the ECS. The coupled biophysical model was used to hindcast the blooms and to test the hypothesis proposed in earlier studies that phosphate(PO4 3–) is the first-order decider of the succession. The coupled model successfully reproduced the hydrodynamics(as described in a companion paper by Sun et al.(1), the spatiotemporal distribution of the chlorophyll a(Chl a) concentration, and the species succession reasonably well. By analyzing the effects of different factors on the surface Chl a distribution, we confirmed that the offshore boundaries of the blooms were confined by PO4 3–. In addition, we suggest that surface wind fields may modulate the horizontal distribution of blooms. Thus, during the dispersal of blooms, surface winds coupled with PO4 3– may control the succession of blooms in the ECS. The proposed coupled model provides a benchmark to facilitate future improvements by including more size classes for organisms, multiple nutrient schemes, and additional processes.  相似文献   
3.
波浪对漂浮式潮流能水轮机的水动力性能具有重要的影响,论文采用切片理论建立和三维水轮机无辐射运动时立轴潮流水轮机水动力载荷近似计算公式,计算分析了浪流同向条件下,海能1号2×150 k W漂浮式潮流电站两叶片固定偏角立轴水轮机在波浪中的水动力载荷。计算结果表明,波浪中潮流水轮机水动力具有双频特性;水轮机工作工况下,每增加1 m波高,水轮机极限载荷增加27%,在相同波高条件下,主轴极限载荷随波长的增加而增大。  相似文献   
4.
近年来,东海原甲藻赤潮在我国东海近岸海域频繁发生。本研究利用生物-物理耦合模型对发生于2005年的东海原甲藻赤潮进行后报模拟,并对控制其起始与发展的因素展开研究。该模型由东海原甲藻种群动力学模型与多层嵌套的水动力模型组合。通过对比模拟结果与室内实验结果,证实种群动力学模型能够很好地重现东海原甲藻在不同光照与磷营养限制条件下的生长过程,同时能够再现藻细胞内部磷含量及藻类对外部营养盐浓度的影响。耦合模型能够较好地再现模拟海域水动力(见Sun et al.,2016)与东海原甲藻赤潮的时空分布。模拟的赤潮发展过程与此前研究中的观测结果一致,且模拟结果表明模型能够捕捉到赤潮初期种群的次表层孕育现象。随后模拟结果被用于诊断决定赤潮垂直分布的决定性因素,结果表明磷酸盐是控制这一现象的关键因素。同时,表层风场在决定赤潮的分布中扮演着重要角色。模拟结果强调了营养盐限制在东海原甲藻次表层孕育及消散过程中的作用,本文所建立的耦合模型需要进一步优化并应用于其它条件下东海原甲藻赤潮的研究中。  相似文献   
5.
Nutrient-controlled growth of Skeletonema costatum : an applied model   总被引:1,自引:0,他引:1  
To model Skeletonema costatum blooms and their relationship with environmental parameters in situ, a S. costatum-specifi c zero-dimensional box model based on the mechanistic model Eco3M was established using physiological features. The parameters were calibrated using experimental counterparts, and simulations were compared with published laboratory fi ndings. The resulting normalized objective function(NOF) values are less than 1.0(and in most cases less than 0.58) and the values for the slope γ(between 0.656 7–1.127 4) and R 2(between 0.806 8–0.971) are close to 1.0 for most of the sub-fi gures. This indicates good agreement between simulated and measured data and suggests that the model reproduces the general characteristics of S. costatum growth and use of nutrients under different N- or P-limiting conditions. The model is appropriate for further applications and can be used to test more scenarios using other nutrients.  相似文献   
6.
初步研究了一株米氏凯伦藻对褶皱臂尾轮虫(Brachionus plicatilis)、卤虫(Artemia salina)幼体和黑褐新糠虾(Neomysis awatschensis)的毒性效应和机制。研究发现米氏凯伦藻(Karenia mikimotoi)在较低密度下就能明显减少轮虫的种群数量,24hEC50仅为20个/mL左右;该藻的各组分毒性比较结果显示,只有藻液和细胞重悬液有这种毒害作用,而去藻过滤液和藻细胞破碎液的影响不明显,表明这种毒害作用可能是由于活的藻细胞引起的;在米氏凯伦藻中卤虫和黑褐新糠虾的存活数量也明显下降。结果表明,米氏凯伦藻赤潮可能通过直接影响存活从而对浮游动物产生影响。  相似文献   
7.
提出一种利用集体土地两权发证数据拓扑关系计算界址线与附着物的内中外关系和宗地四邻关系的方法,同时完成实体属性挂接,自动生成调查表。  相似文献   
8.
李宜龙  曾敏  孙科  罗吉 《海洋测绘》2014,34(6):40-42
数字滤波器是影响航空重力测量数据处理成果质量的关键技术之一。分析比较了布莱克曼窗函数滤波和高斯滤波的特点,并利用实测数据对各类滤波器的性能进行了实际验证。结果表明,航空重力测量数据处理中高斯滤波和布莱克曼滤波的精度相当,高斯滤波略优,表明高斯滤波器同样适用于航空重力数据的滤波处理。  相似文献   
9.
By combing satellite-derived ice motion and concentration with ice thickness fields from a popular model PIOMAS we obtain the estimates of ice volume flux passing the Fram Strait over the 1979–2012 period. Since current satellite and field observations for sea ice thickness are limited in time and space, the use of PIOMAS is expected to fill the gap by providing temporally continued ice thickness fields. Calculated monthly volume flux exhibits a prominent annual cycle with the peak record in March(roughly 145 km3/month) and the trough in August(10 km~3/month). Annual ice volume flux(1 132 km~3) is primarily attributable to winter(October through May) outflow(approximately 92%). Uncertainty in annual ice volume export is estimated to be 55 km~3(or 5.7%). Our results also verified the extremely large volume flux appearing between late 1980 s and mid-1990 s. Nevertheless, no clear trend was found in our volume flux results. Ice motion is the primary factor in the determination of behavior of volume flux. Ice thickness presented a general decline trend may partly enhance or weaken the volume flux trend. Ice concentration exerted the least influences on modulating trends and variability in volume flux. Moreover, the linkage between winter ice volume flux and three established Arctic atmospheric schemes were examined. Compared to NAO, the DA and EOF3 mechanism explains a larger part of variations of ice volume flux across the strait.  相似文献   
10.
北极地区不同冰龄的海冰厚度变化研究   总被引:1,自引:0,他引:1  
In this study, changes in Arctic sea ice thickness for each ice age category were examined based on satellite observations and modelled results. Interannual changes obtained from Ice, Cloud, and Land Elevation Satellite(ICESat)-based results show a thickness reduction over perennial sea ice(ice that survives at least one melt season with an age of no less than 2 year) up to approximately 0.5–1.0 m and 0.6–0.8 m(depending on ice age) during the investigated winter and autumn ICESat periods, respectively. Pan-Arctic Ice Ocean Modeling and Assimilation System(PIOMAS)-based results provide a view of a continued thickness reduction over the past four decades. Compared to 1980 s, there is a clear thickness drop of roughly 0.50 m in 2010 s for perennial ice. This overall decrease in sea ice thickness can be in part attributed to the amplified warming climate in north latitudes. Besides, we figure out that strongly anomalous southerly summer surface winds may play an important role in prompting the thickness decline in perennial ice zone through transporting heat deposited in open water(primarily via albedo feedback) in Eurasian sector deep into a broader sea ice regime in central Arctic Ocean. This heat source is responsible for enhanced ice bottom melting, leading to further reduction in ice thickness.  相似文献   
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