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871.
环境刑事诉讼上诉期间的生态环境修复行为逐渐被一些地方法院在二审程序中作为从宽减刑的情节考察。虽然此举有益于激励环境刑事被告人积极履行环境恢复义务,然则在未有明文规定的先决条件下贸然将其纳入从宽量刑考量,也许会打破传统二审救济纠错的应然功能设计,使得环境刑事诉讼二审功能的实现存在矛盾偏差。由是对于上诉期间发生的生态修复行为的法律定性,应明确归属于判决后刑罚执行阶段的减刑情节予以考量,并且为配合化解此类矛盾,我国须及时制定相应的专门法规、适用原则和配套制度措施,从而最大限度发挥生态修复行为在环境刑事诉讼中的效用。 相似文献
872.
Patterns and drivers of CH4 concentration and diffusive flux from a temperate river–reservoir system in North China 下载免费PDF全文
Fanyan Yang Jicheng Zhong Shaoming Wang Xiaokang Hu Hongwei Wang Mengyao Tang Min Zhang Chuanzhe Sun Lei Zhang 《环境科学学报(英文版)》2022,34(6):184-197
Freshwater reservoirs are regarded as an important anthropogenic source of methane (CH4) emissions. The temporal and spatial variability of CH4 emissions from different reservoirs results in uncertainty in the estimation of the global CH4 budget. In this study, surface water CH4 concentrations were measured and diffusive CH4 fluxes were estimated via a thin boundary layer model in a temperate river–reservoir system in North China, using spatial (33 sites) and temporal (four seasons) monitoring; the system has experienced intensive aquaculture disturbance. Our results indicated that the dissolved CH4 concentration in the reservoir ranged from 0.07 to 0.58 µmol/L, with an annual average of 0.13 ± 0.10 µmol/L, and the diffusive CH4 flux across the water–air interface ranged from 0.66 to 3.61 μmol/(m2•hr), with an annual average of 1.67 ± 0.75 μmol/(m2•hr). During the study period, the dissolved CH4 concentration was supersaturated and was a net source of atmospheric CH4. Notably, CH4 concentration and diffusive flux portrayed large temporal and spatial heterogeneity. The river inflow zone was determined to be a hotspot for CH4 emissions, and its flux was significantly higher than that of the tributary and main basin; the CH4 flux in autumn was greater than that in other seasons. We also deduced that the CH4 concentration/diffusive flux was co-regulated mainly by water temperature, water depth, and water productivity (Chla, trophic status). Our results highlight the importance of considering the spatiotemporal variability of diffusive CH4 flux from temperate reservoirs to estimate the CH4 budget at regional and global scales. 相似文献