The performance of RAMS in representing the convective boundary layer structure in a very steep valley

Data from a comprehensive field study in the Riviera Valley of Southern Switzerland are used to investigate convective boundary layer structure in a steep valley and to evaluate wind and temperature fields, convective boundary layer height, and surface sensible heat fluxes as predicted by the mesoscale model RAMS. Current parameterizations of surface and boundary layer processes in RAMS, as well as in other mesoscale models, are based on scaling laws strictly valid only for flat topography and uniform land cover. Model evaluation is required to investigate whether this limits the applicability of RAMS in steep, inhomogeneous terrain. One clear-sky day with light synoptic winds is selected from the field study. Observed temperature structure across and along the valley is nearly homogeneous while wind structure is complex with a wind speed maximum on one side of the valley. Upvalley flows are not purely thermally driven and mechanical effects near the valley entrance also affect the wind structure. RAMS captured many of the observed boundary layer characteristics within the steep valley. The wind field, temperature structure, and convective boundary layer height in the valley are qualitatively simulated by RAMS, but the horizontal temperature structure across and along the valley is less homogeneous in the model than in the observations. The model reproduced the observed net radiation, except around sunset and sunrise when RAMS does not take into account the shadows cast by the surrounding topography. The observed sensible heat fluxes fall within the range of simulated values at grid points surrounding the measurement sites. Some of the scatter between observed and simulated turbulent sensible heat fluxes are due to sub-grid scale effects related to local topography.     

Structure of turbulent plumes from a momentumless source in a smooth bed

The spatial development of a passive scalar plume is studied within the inhomogeneous turbulence of a boundary layer flow in a recirculating laboratory flume with a smooth bed. The source of the scalar is located flush with the bed, and the low-momentum source design is intended to simulate a diffusive-type scalar release. A weakly diffusive fluorescent dye is used as the scalar. Planar laser-induced fluorescence (PLIF) techniques were used to record the structure of the plume at a spatial resolution of 150 μm. The measured structure of the mean concentration field is compared to an analytical solution for shear-free, homogeneous turbulence. The laboratory plume exhibits spatial development in the mean concentration field that deviates from the self-similar behavior predicted by the analytical solution; this deviation is due to the mean shear and inhomogeneity of the turbulence. In particular, the influence of the viscous sublayer on the plume development is seen to be significant. Nonetheless, the analytical solution replicates some of the features seen in the laboratory plume, and the solution suggests methods of reducing the laboratory data even for cases where the results deviate from the analysis. We also examine the spatial development of the root-mean-square (rms) fluctuating concentration field, and use scalar probability density functions to examine the relationship between the mean and fluctuating concentrations.     

耗散结构理论在土壤科学上应用途径的探索

本文根据耗散结构的基本理论，结合生产实践经验，提出了表征土壤肥力的非线性微分方程：＝（Ｋ－ｂ）ｘ－βｘ２Ｘ─土壤生物活性，ｔ─时间，Ｋ─生物繁殖系数，ｂ─生物死亡系数，β─生物饱和系数．解这个并不复杂的非线性微分方程，便可知道土壤是处于热力学分枝，还是耗散结构分枝．这对研究土壤肥力的动态变化、土壤肥力的分类、土壤的管理、土壤退化的防止等方面有着无法预测的应用前景．     

观音堂库区水温变化对水生态环境影响的分析

本文用径流-库容比数法，对观音堂水库水体水温结构类型进行判断，用经验公式法和代表层水温法对观音堂水库水体水温结构和下泄水温进行了预测，预测结果表明：观音堂水库属分层型水库，在汛期表现出临时混合型的特点，水库下泄水使下游河道水温年内分布趋于均匀．这种水温变化，导致水库水质随水库深度增加而逐渐恶化，对水库下游河段水生生态系统产生不利影响。     

农村产业结构调整问题研究

本文首先对农村产业结构调整的相关概念进行了阐述.其次,分析和归纳了判断农村产业结构合理化的标准以及农村产业结构变动的影响因素.     

围栏禁牧对川西北亚高山高寒草甸群落结构的影响

围栏禁牧4a后,与放牧草地相比较:1)围栏草地物种数量有所下降,群落内出现物种27种,而长期放牧草地为33种.2)围栏草地物种平均高度较高,为20.23cm,群落分层现象明显;放牧草地物种平均高度仅为8.14cm,群落无分层现象.3)围栏草地内,杂草类的盖度(98%)大于禾草类的盖度(14%);放牧草地上,杂草类的盖度(53%)小于禾草类的盖度(56%)。4)围栏草地以禾草为主的优良牧草的生产能力(35.24g/m2)低于放牧草地的生产能力(75.47g/m2).5)围栏草地的地上生物量(272.64g/m2)和地下0～30cm生物量(801.61g/m3)都高于放牧草地的地上生物量(184.84g/m2)和地下0～30cm生物量(683.82g/m3).研究结果表明,围栏草地具有比放牧草地更复杂的群落结构,但其物种组成和优良牧草的生产能力,都低于放牧草地.     

Population structure and historical demography of the thorny skate (<Emphasis Type="Italic">Amblyraja radiata</Emphasis>, Rajidae) in the North Atlantic

Population genetic structure of the thorny skate (Amblyraja radiata) was surveyed in >300 individuals sampled from Newfoundland, Iceland, Norway, the Kattegat and the central North Sea. A 290-bp fragment of the mt cytochrome-b gene was first screened by SSCP. Sequences of SSCP haplotypes revealed 34 haplotypes, 14 of which were unique to Iceland, 3 to Newfoundland, 1 to Norway and 3 to the Kattegat. The global F _ST was weak but significant. Removal of the two Kattegat locations, which were the most differentiated, resulted in no significant genetic differentiation. Haplotype diversity was high and evenly distributed across the entire Atlantic (h = 0.8) with the exception of the North Sea (h = 0.48). Statistical parsimony revealed a star-like genealogy with a central widespread haplotype. A subsequent nested clade analysis led to the inference of contiguous expansion with evidence for long distance dispersal between Newfoundland and Iceland. Historical demographic analysis showed that thorny skates have undergone exponential population expansion that started between 1.1 million and 690,000 years ago; and that the Last Glacial Maximum apparently had little effect. These results strongly differ from those of a parallel study of the thornback ray (Raja clavata) in which clear structure and former refugial areas could be identified. Although both species have similar life history traits and overlapping ranges, the continental shelf edge apparently does not present a barrier to migration in A. radiata, as it does for R. clavata.     

River water quality management model using genetic algorithm

Conventional mathematical programming methods, such as linear programming, non linear programming, dynamic programming and integer programming have been used to solve the cost optimization problem for regional wastewater treatment systems. In this study, a river water quality management model was developed through the integration of a genetic algorithm (GA). This model was applied to a river system contaminated by three determined discharge sources to achieve the water quality goals and wastewater treatment cost optimization in the river basin. The genetic algorithm solution, described the treatment plant efficiency, such that the cost of wastewater treatment for the entire river basin is minimized while the water quality constraints in each reach are satisfied. This study showed that genetic algorithm can be applied for river water quality modeling studies as an alternative to the present methods.     

中亚热带丝栗栲次生林群落高度级结构分析

以高度级为参考坐标，应用衡量优势种群及群落结构动态的失稳率、群落垂直空间的分享度、α—多样性及群落高度级梯度β—多样性等指标对中亚热带丝栗栲次生林群落高度级结构特征及其动态进行分析评价。结果表明：丝栗栲群落及其优势种群个体数、群落物种数和种对级的分享度随高度级增加都呈下降趋势；各高度级物种数和个体数呈明显的正相关关系；级间失稳率显示，群落在第2、3、6、7高度级呈增长趋势，第4、5高度级呈衰退趋势，群落整体具有增长性结构；群落随高度级形成丰富度指数(dMa)、Shannon—Wiener指数(H)逐渐降低，均匀度指数(J)先增后减的变化趋势；随高度级梯度的增加，群落相邻高度级间Whittaker指数(βw)呈上升趋势，而Mofisita—Horn指数(CMH)呈不规则地跳跃式变化，表现了共有种在群落不同高度级的数量差异。图3表2参15。