水利建设可持续发展刍议

首先分析了水利建设与可持续发展的关系,即可持续发展对水利建设提出了新要求、丰富了新思路,水利建设实践推动了水利可持续发展研究,并基于此提出水利建设可持续发展思路,即树立可持续发展意识,推进水利建设制度创新;人水协调,加强水利现代化建设.     

水利施工的大体积混凝土抗裂技术

混凝土是水利施工中的主要的应用材料之一，为了保证水利施工中的安全与质量，必须保证混凝土的质量。文章全面分析了大体积混凝土产生裂缝的原因，并给出了相应的控制方法。     

河南长江流域防护林工程水土保持效益评价

涵养水源和保育土壤是森林的主要生态功能。通过采用森林生态系统服务功能实物量、价值量评估方法对长防林工程实施区域森林的水土保持效益进行的评价,结果表明,长防林工程实施后林地可调节水量12.936亿m3,固土0.135亿t,林地的水土保持效益价值达126.247亿元。经过20年的长防林工程建设,项目区内森林资源快速增长,水土流失面积大幅度减少,工程建设对生态环境的改善起到了明显的作用。     

Decreasing of methanogenic activity in paddy fields via lowering ponding water temperature: A modeling investigation

Methane (CH₄) is a potent greenhouse gas and the huge CH₄ fluxes emitted from paddy fields can prejudice the eco-compatibility of rice cultivation. CH₄ production in submerged rice crops is known to be highly influenced by water temperature. Hence, lowering ponding water temperature (LPWT) could be an option to mitigate CH₄ emissions from paddy environments when it is possible either to irrigate with slightly colder water or to increase ponding water depth. However, paddy soil is a complex environment in which many processes are simultaneously influenced by temperature, leading to a difficult prediction of LPWT effects. For this reason, LPWT efficiency is here theoretically investigated with a one-dimensional process-based model that simulates the vertical and temporal dynamics of water temperature in soil and the fate of chemical compounds that influence CH₄ emissions. The model is validated with literature measured data of CH₄ emissions from a paddy field under time-variable temperature regime. Based on modeling results, LPWT appears promising since the simulated reduction of CH₄ emissions reaches about −12% and −49% for an LPWT equal to −5 °C during the ripening stage only (last 30 days of growing season, when rice is less sensitive to temperature variations) and −2 °C over the whole growing season, respectively. LPWT affects CH₄ emissions either directly (decreasing methanogenic activity), indirectly (decreasing activity of bacteria using alternative electron acceptors), or both. The encouraging results provide the theoretical ground for further laboratory and field studies aimed to investigate the LPWT feasibility in paddy environments.     

Limited effects of land use on soil dissolved organic matter chemistry as assessed by excitation–emission fluorescence spectroscopy and molecular weight fractionation

Dissolved organic matter (DOM) in soil solution represents a complex mixture of organic molecules and plays a central role in carbon and nitrogen cycling in plant–microbial–soil systems. We tested whether excitation–emission matrix (EEM) fluorescence spectroscopy can be used to characterize DOM and support previous findings that the majority of DOM is of high molecular weight (MW). EEM fluorescence spectroscopy was used in conjunction with MW fractionation to characterize DOM in soil solution from a grassland soil land management gradient in North Wales, UK. Data analysis suggested that three distinct fluorescence components could be separated and identified from the EEM data. These components were identified as being of humic‐like or fulvic‐like origin. Contrary to expectations, the majority of the fluorescence signal occurred in the small MW (<1 kDa) fraction, although differences between soils from the differently managed grasslands were more apparent in larger MW fractions. We conclude that following further characterization of the chemical composition of the fluorophores, EEM has potential as a sensitive technique for characterizing the small MW phenolic fraction of DOM in soils.     

新疆恒源煤矿新近系水体采动等级评价

指出了恒源煤矿侏罗系煤系地层基本无水,主要充水水源为新近系独山子组的孔隙-裂隙含水层,但是主井筒开拓时,开始涌水量很小,继续向下开拓时,井筒涌水量超过1000m3/h。计算了煤层"两带"高度和新近系含水层与下覆煤系地层间距,研究表明:煤系地层与新近系水体间并无直接的水力联系,具体的涌水来源尚无定论,估算矿井的最大涌水量为160.74m3/h,正常涌水量为53.58m3/h。     

林地水土保持功能持续提高的机制及对策

通过对不同林地水土保持功能分析得出,其发展过程可分为成长期、成熟期和减退期,并定义成熟期为可持续发展期。分析了影响水土保持功能持续提高的环境分配系数r和环境利用系数k,认为r是林地中光、水、肥分配的参数,k为光、水、肥利用的参数。林地水土保持功能的持续提高,应通过调整r和k,即调控林地的树种组成、林分层次和林分密度,形成合理的林分结构,保持成熟期的持续发展。并在此基础上提出了林地水土保持功能持续提高的相应对策。     

新疆林业海量影像数据管理系统建设

介绍新疆林业海量影像数据管理系统建设的关键技术和系统功能。系统通过对多源、多时相、多分辨率的影像数据的统一化、标准化的组织和管理,提供在线影像浏览、查询、对比分析和影像下载等功能,实现了海量影像数据的管理与共享。     

Short‐term releases of CO2 from newly mixed biochar and calcareous soil

The work aimed to quantify native organic C mobilized in one calcareous soil in the 21 days after addition of biochar at a range of large to very large applications. The experiment was carried out in unplanted microcosms, and CO₂ flux was used as a measure of net mineralization. A rapid methodological approach, which does not require ¹³C as a tracer, was used to assess any priming effects induced by the biochar. The amount of CO₂‐C mobilized was small relative to the amount of biochar C and proportional to the amount of the biochar added. The additional CO₂‐C was similar to the content of the water‐soluble organic carbon in the biochar added with each application. No interaction with native soil C, that is priming effect, was observed.     

基于叶气温差的生育中期冬小麦水分亏缺诊断研究

为了获取叶片尺度基于叶气温差的冬小麦生育中期水分亏缺诊断阈值,分析了冬小麦叶气温差的典型日变化及其与土壤水分、空气温度及太阳辐射等因子的相互关系,揭示了冬小麦叶气温差对光合气体交换参数的影响,确定了冬小麦叶片水分利用效率较适宜的非气孔限制值及叶气温差范围。结果表明,冬小麦叶气温差在不同的土壤水分条件下表现出不同的日变化规律,随光量子通量增加而升高,随土壤水分、气温增加而降低;4、5和6月冬小麦叶片水分利用效率较适宜的非气孔限制值范围分别为0.7~1.3、1.1~2.0和0.9~1.5,叶气温差控制范围分别为-1.2~0.4、-1.5~-1和-1.25~-0.9℃。