构建黑龙江省粮食利益补偿机制研究初探

黑龙江省是国家粮食主产区之一,近年来粮食生产取得了显著成效,然而,黑龙江省粮食主产区在自身区域经济发展中因政策性原因遭遇经济发展瓶颈。本文从分析保障国家粮食安全和发展区域经济的关系入手,论证了保障国家粮食安全和发展区域经济的对立统一关系,并着重分析了黑龙江省粮食主产区现在面临的区域经济发展窘境,结合十七届三中全会提出的加快实现粮食增产、农民增收、财力增强相协调,充分调动农民种粮、地方抓粮积极性的要求,提出了构建以粮食安全保障基金、商品粮调销补偿基金、耕地保护基金为主的黑龙江省粮食主产区利益补偿建议,最终实现保障国家粮食安全、富民增收、区域经济协调发展的目标。     

疏勒河上游地表水水化学主离子特征及其控制因素

在系统收集了疏勒河流域上游河水、地下水、降水和冰雪融水水样的基础上,综合运用描述性统计、Gibbs图和Piper阴阳离子三角图等方法,对疏勒河上游地表水中主离子组成特征及其控制因素进行了分析.结果表明,流域内不同水体(大气降水、河水和地下水)之间的主离子组成以及水化学类型差异显著.河水TDS的变化范围为51.7~432.3 mg·L-1,平均值为177.7 mg·L-1;河水中阳离子Ca2+、Mg2+的百分比为45%和31%,优势阴离子为HCO-3,占阴离子总量的75%,河水的水化学类型主要为HCO-3-Ca2+-Mg2+型;河水中主离子浓度值介于大气降水和地下水之间,并且十分接近地下水浓度,说明地表水同时受大气降水和地下水补给并主要依靠地下水补给;地表水样品的水化学组成落在Gibbs分布模型的中翼偏左端,表明研究区的水化学离子组成受到岩石风化作用和蒸发结晶作用的共同影响,且岩石风化作用对水化学离子组成的影响更加显著.     

蛤蟆通河流域地下水化学特征及控制因素

为研究蛤蟆通河流域水化学特征及主要离子来源,2017年先后采集地下水样品59组,综合运用数理统计、Piper三线图、Gibbs模型和离子比等方法,分析了蛤蟆通流域地下水的水文地球化学特征,并探讨了蛤蟆通流域的水化学演化规律及主要离子来源.结果表明,该区地下水阳离子以Ca~(2+)为主,占阳离子总量的质量分数为22. 1%～72. 4%,平均为48. 7%;阴离子以HCO_3~-为主,占阴离子总量的质量分数为35. 3%～97. 5%,平均为80%; TDS介于93. 3～521. 1 mg·L~(-1),平均值为219. 1 mg·L~(-1),均为淡水;地下水类型以HCO_3-Ca、HCO_3-Ca·Mg和HCO_3-Ca·Na型水为主;地下水样品均分布在Gibbs模型左中部,说明该流域水化学离子组成受岩石风化作用控制;通过离子来源分析,该区主要离子来源于硅酸盐岩和碳酸盐岩的风化溶解.     

黄海西部大气湿沉降(降水)的pH与主要酸碱离子的关系

对黄海西部的千里岩、青岛的麦岛两个降消要样点１９９７、１９９８丙年所收集的１１３个降 Ｈ＾＋、ＮＨ４＾＋、Ｋ＾＋、Ｎａ＾＋、Ｃａ＾２＋、Ｍｇ＾２＋、Ｆ＾－、Ｃｌ＾－、ＮＯ３＾－、ＳＯ４＾２－共１０种离子成分的含量，分别用ＮＡ＾＋、Ｍｇ＾２＋、Ｃａ＾２＋＋ＮＨ４＾＋）／（ＮＯ３＋ｎｓａＳＯ４＾２－、ｃｍｓｓＳＯ４＾２－（ｎｓｓＳＯ４＾２－）的相关分析。结果表明：（１）以Ｍｇ＾２＋作为参考元素计算得到     

我国重大活动环境空气质量监测预报评估技术体系的发展与思考

通过总结南京青年奥林匹克运动会、二十国集团领导人峰会、金砖国家领导人第九次会晤、中国国际进口博览会、第七届世界军人运动会等重大活动环境空气质量保障工作经验,简述近年来中国重大活动环境空气质量监测预报评估技术的进展以及所发挥的作用。结合城市环境精细化管控和未来我国"十四五"环境空气质量持续改进的需求,提出在监测网络、监测技术、排放清单、预测预报产品和保障机制等方面有待提升的建议。     

Toward an improved ecosystem based management approach: incorporating catchment characteristics into better management and planning of the Great Barrier Reef marine ecosystem

Discharge from the Great Barrier Reef Catchment (GBRC) is considered the second most serious threat to the Great Barrier Reef, Australia. Utilising principal component analysis (PCA) and cluster analysis (CA), this research aimed to assess the variability and co-variation of 28 water basins (WBs) within the GBRC, in order to improve the institutional arrangements and regulation of water quality and increase collaboration horizontally between management organisations, and vertically between government tiers. Water basin variability was measured by nine variables: size (ha), population, agricultural land use (ha), number of major water storages, major rivers and major towns, total nitrogen exported (T/yr), total phosphorus exported (T/yr) and herbicide use (ha). The Fitzroy WB, with PC scores of 7.0081, 2.2897 and ?1.6504, was identified as the most dissimilar and therefore needing to be managed differently. Many WBs within the same regions were very dissimilar to each other, indicating that current management practices, based largely on geographic location, are unlikely to be the most efficient and effective. Instead, managing groups of WBs with similar geo-political properties (determined by the CA) could be more effective and efficient. Coordination and collaboration are key to successful ecosystem based management, therefore managing similar WBs together through inter-NRM (natural resource management) agreements, irrespective of their geographical location, facilitates management bodies building strong, cooperative working relationships.     

MONTHLY RUNOFF DISTRIBUTION RELATED TO BASIN GEOGRAPHY1

ABSTRACT: Mean monthly runoff from ungaged drainage basins that have significant snowpacks each year can be estimated quite well by assuming that the time duration between snowfall and snowmelt is the predominant factor in temporal runoff distribution. That time span is related to basin temperatures which are, in turn, functions of basin elevation and latitude. Regional hydrologic analyses of gaged basin data create regression equations for estimating runoff distribution by month. These equations then can be applied to ungaged basins. Basin latitude and mean elevation are two independent variables that can be used in estimating monthly runoff distributions.     

华北城市地区潜水中主要离子含量变化的反应途径模拟

近三十年来，由于污染，华北城市地区潜水中主要离子如ＣＡ＾２＋、Ｍｇ＾２＋等含量逐年升高，影响工农业生产，本采用反应途径模拟的方法对上述情况进行了研究，作共设计了７种反应途径，分别模拟了含碳酸盐或硅酸盐、铝硅酸盐较丰富地区地下水中盐效应和ＣＯ２分压升高对基主要离子含量的影响，模拟过程中考虑了２２种化学反应，３３种存在形式（包括气体、固体）。结果表明，盐效应和ＣＯ２分压升高对地下水中Ｃａ＾２＋、Ｍ     

Floods in southern Portugal: their physical and human causes,impacts and human response

Floods have been the most deadlynatural disasters in Portugal during the lastcentury, followed by earthquakes. The typeof flood known as a `progressive flood'mainly affects the larger basins, such asthat of the Tagus River, and results in alarge inundated area. These floods arecaused by heavy rains associated with awesterly zonal circulation that may persistfor weeks. The system of dams within thebasin reduces the frequency of flooding,but cannot `tame' the river. The dam systemhas even contributed to an increase in thepeak flow, as in the 1979 flood.Nevertheless, these floods are not a dangerfor the human population. In contrast, flashfloods are more dangerous and deadlier thanprogressive floods, as demonstrated in 1967and 1997. They affect the small drainagebasins and are caused by heavy andconcentrated rainfall, created byconvective depressions (active cold poolsor depressions caused by the interactionbetween polar and tropical air masses),active in the south of the country, in theLisbon region, Alentejo and the Algarve.Deforestation, soil impermeability, chaoticurbanization, building on floodplains, theblockage of small creeks or theircanalisation, and the building of walls andtransverse embankments along the smallcreeks all contribute to the aggravation ofthis kind of flood.     

火山断陷盆地的边缘成矿论

火山断陷盆地是构造-岩浆-地热体系的最活跃场所。大中型热液矿床往往赋存于盆地边缘。高渗透构造破碎带、基底和火山盖层建造的相应组合、多阶段次火山岩的侵入、配套的水文地质环境构成了盆边热源、矿源、水源、矿质沉淀空间的最佳匹配条件。因此．盆地边缘作为矿床预测和靶区优选的显著目标值得找矿者的高度重视。