雷州半岛桉林-砖红壤水分动态变化特征研究

根据定位观测数据,对雷州半岛浅海沉积物发育的桉林地砖红壤水分状况及其动态变化进行了初步探讨.结果表明,受水分蒸发量大等因素的影响,0～100 cm土层月均贮水量较低;主要受降雨分布的影响,土壤水分呈明显的季节性变化特征且季节性干旱时间较长,8～     

南极法尔兹半岛植被土壤CH_4通量特征

应用密闭箱法首次测定了南极法尔兹半岛苔藓、地衣植被土壤CH4 排放通量 ,并估算了该半岛植被土壤在夏季 2个月内CH4 的排放总量 .结果表明 :在晴好天气条件下 ,苔藓土壤CH4 排放通量可能呈现双峰型变化特征 ;而在雨、雪等复杂多变的天气条件下 ,CH4 通量变化无规则 ,存在较大的时空变化 ,且与温度的响应关系不明显 ;苔藓土壤CH4 通量夏季变化的主要影响因子是温度 ,同时还受降水的影响 .苔藓土壤吸收CH4 总量为 0 6 6 5 3× 10 2 kg ;地衣土壤吸收CH4 总量为 0 76 0 3×10 2 kg .由此可见 ,该半岛苔藓、地衣植被土壤起着大气CH4 汇的作用     

桉林-砖红壤水分性能特征研究

根据室内测定资料,对雷州半岛桉林地砖红壤水分性能进行了探讨。结果表明,与自然植被下的砂页岩赤红壤比较,浅海沉积物桉林-砖红壤导水性、持水能力及供水能力均较低。在同样的吸力下,土壤持水量较少,在同样的吸力段,土壤释放的水量较少;玄武岩桉林-砖红壤持水能力较高,但导水性和供水能力较低。通径分析结果表明,浅海沉积物桉林-砖红壤持水能力较低主要受粘粒较少影响,其水分的有效性较低主要与其有机质的较少有较大关系;玄武岩桉林-砖红壤持水能力较高而水分的有效性较低,主要受其粘粒含量较高、有机质含量较低的制约。     

雷州半岛旱地砖红壤非点源氮、磷淋溶损失模拟研究

大量施用化学肥料所引起的养分淋失和环境污染正逐渐受到人们的重视。通过土柱模拟氮、磷素养分淋溶试验．研究了不同施肥处理下砖红壤氮、磷素淋溶损失特点。试验结果表明，随着尿素用量的增加，渗漏水中NH4^＋-N质量浓度和TN淋失量也相应增加，而NO3^--N的质量浓度变化幅度较大，渗漏水中氮素淋失形态主要是以NO3^--N为主。由于土壤磷素很难移动，所以TP累积淋失量非常少，氮、磷肥混施对非点源氮、磷素的淋失都有影响，其中过量磷肥配合尿素施用可以增加土壤中NH4^＋-N、NO3^- -N、TN的淋失程度。     

Forest cover dynamics in the Selva Maya of Central and Southern Quintana Roo,Mexico: deforestation or degradation?

ABSTRACT

Forest cover dynamics (1993-2018) was assessed in two regions on the Yucatan Peninsula: Zona Maya (ZM), 67% indigenous with shifting cultivation and community forestry; and Bacalar–Rio Hondo (BRH), mainly commercial agriculture and pastureland. Degradation (12,915 ha y^?1) exceeded deforestation (5882 ha y^?1) and was worse in BRH. In BRH there was a net forest loss (?1.6% y^?1) associated with pastureland and commercial agriculture. In ZM, mature forest recovery (1.4% y^?1) and dynamic forest cover (continuous loss and gain) were associated with shifting cultivation. Changes were more intense during 2011–2018 and gains of mature forest in ZM and deforested areas in BRH targeted secondary vegetation. Fragments of mature and secondary vegetation decreased, and connectivity improved in ZM, but opposite trends occurred in BRH. Reporting and monitoring deforestation using Global Forest Watch data is inadequate since 62% of forest cover loss represent degrading or recovering forest cover.     

雷州无瓣海桑群落7种元素的生物累积和循环

在雷州市附城镇岚北人工生态恢复的 7a生无瓣海桑群落生物量调查的基础上 ,对所采集的无瓣海桑进行了植物体各组分样品的灰分和元素含量测定与循环分析 ,结果表明 :无瓣海桑植物体不同组分的灰分含量范围为 2 .2 7%～ 2 6 .4 1% ,以细根的含量最高 ,枯枝的含量最低 .植物体各组分中 7种元素质量分数范围分别为K 0 .11%～ 1.5 6 % ,Na0 .11%～ 1.6 6 % ,Ca 0 .2 0 %～ 2 .6 6 % ,Mg 0 .15 %～ 1.5 9% ,Fe 0 .0 4× 10 -3 ～ 9.6 4× 10 -3 ,Zn 0 .0 5× 10 -4～ 1.0 3× 10 -4,Cu0 .16× 10 -5～ 1.5 0× 10 -5.其加权平均的富集系数为 0 .0 5～ 9.70 ,其中Ca >K >Cu >Na >Mg>Zn >Fe .群落现存生物量中的累积储量分别为K 10 9.76gm-2 ,Ca 138.89gm-2 ,Na 86 .5 7gm-2 ,Mg 81.0 7gm-2 ,Fe 13.139gm-2 ,Zn 0 .4 83gm-2 ,Cu 0 .10 8gm-2 .群落 2 0 0 1年的元素存留累积储量分别为Ca4 1.6 8gm-2 ,K 37.2 4gm-2 ,Mg 2 7.33gm-2 ,Na2 5 .5 6gm-2 ,Fe 4 .2 75gm-2 ,Zn 0 .188gm-2 ,Cu 0 .0 39gm-2 .2 0 0 1年归还量分别为Ca 2 8.5 9gm-2 ,K 16 .83gm-2 ,Mg 12 .0 7gm-2 ,Na 11.5 8gm-2 ,Fe 0 .916gm-2 ,Zn 0 .14 1gm-2 ,Cu 0 .0 2 6gm-2 .年吸收量分别为Ca 70 .2 7gm-2 ,K 5 4 .0 7gm-2 ,Mg 39.4 0gm-2 ,Na 37.1     

基于P-S-R概念模型的生态环境承载力评价指标体系研究——以山东半岛为例

结合山东半岛生态环境现状,根据该区域的社会经济和环境特点,采用压力-状态-响应(P-S-R)概念模型,选取了25项指标构建了其生态环境承载力评价指标体系,运用层次分析法(AHP)确定各指标权重,然后将模糊数学综合评价的理论和方法应用于山东半岛生态环境承载力的评估,对2009及2012年度山东半岛6个城市的生态环境承载力做出评价.评价结果为威海市生态环境承载力为Ⅰ级优,承载力稳中有升,青岛、烟台、日照市为Ⅱ级良,青岛、烟台承载力略升,日照略有下降,潍坊市为Ⅲ级中等,承载力有所下降,东营市由Ⅳ级差变为Ⅲ级中等,承载力明显好转.同时,并对每个城市的生态环境承载力做了分析说明,以期为推进生态文明建设提供科学依据.     

Pollution-induced successions in forests of the Kola Peninsula

Trends of changes in the successional status of northern taiga forests exposed to technogenic pollution in the Kola Peninsula are discussed. Main studies of digression in spruce and pine forests are characterized on the basis of the dynamics of species composition of phytocenoses and chemical composition of atmospheric fallout, soils, and dominant plants.     

GEOCHEMICAL INTERPRETATIONS OF GROUNDWATER FLOW SYSTEMS1

ABSTRACT. Interest in the geochemistry of groundwater is increasing owing to the great number of current projects involving underground liquid waste storage, artificial recharge of potable water, accidental contamination of groundwater bodies, sanitary landfills, and pollution monitoring. Geochemical techniques used to facilitate the understanding of a groundwater system range from extremely simple to those requiring sophisticated theories, equipment, and procedures. An interpretation of the simple trilinear diagram for samples collected from the Yucatan Peninsula of Mexico provided evidence that the fresh-water body was only a few tens of meters thick and was underlain everywhere by an extensive body of salt water. A geochemical technique that has been used effectively to identify the source of salt water in coastal aquifers is measurement of the carbon-14 concentrations. Carbon-14 has been used in a regional carbonate aquifer to determine the velocity of groundwater movement, rates of chemical reactions, and distribution of hydraulic conductivity. The application of principles of irreversible thermodynamics to groundwater systems provides a basis for constructing models which permit prediction, over both time and space, of changes in head distribution and chemical character of the water resulting from imposed stresses on the system. In essence, proper application of irreversible thermodynamics combines the potential theory of Hubbert with principles of reversible chemical thermodynamics, such as solution of carbonate minerals, to describe and explain controlling chemical reactions and processes of groundwater systems.     

山东半岛城市群相对资源承载力与竞争力研究

以山东半岛城市群为例，采用相对资源承载力的研究思路和计算方法，计算分析了其2000-2004年相对土地资源承载力、相对经济资源承载力和综合承载力及其演化过程。研究表明：①山东半岛城市群的土地资源对综合承载力的贡献大于经济资源，是山东半岛城市群人口的主要承载资源；②山东半岛城市群的综合承载力超过实际人口数量，处于相对富余状态；③相对资源承载力的地区差异较明湿，淄博、日照处于超载状态，其它处于富余状态；④相对土地资源承载力与相对经济资源承载力的小协调发展是提升山东半岛城市群竞争力需要重点解决的问题。