福寿螺的生物防治现状、问题与对策

福寿螺(Pomacea canaliculata)作为一种世界性入侵生物,引入中国已有30余年,现已在中国南方十多个省市大面积分布,造成不可估量的经济损失和生态灾害。本文系统总结了福寿螺生物防治中的天敌资源种类,涵盖了腹足纲、环带纲、昆虫纲、软甲纲、辐鳍鱼纲、爬行纲、鸟纲、哺乳纲等8个类别。并从天敌的引入、研发、利用等方面以及福寿螺应对天敌的防御策略上指出了目前福寿螺生物防治中面临的主要问题。最后对其未来的研究提出了展望,即重点从原产地天敌、寄生性天敌、微生物、生物防治植物和本地经济动物等方面进行筛选,以期为利用中国丰富的生物资源进行福寿螺的生物防治提供参考。     

森林转换对地表径流可溶性有机碳输出浓度和通量的影响

米槠次生林转换成米槠人工幼林和米槠人工促进天然更新幼林(以下简称"人促幼林")后,以这三种森林类型为研究对象,连续监测每次降雨后地表径流量及径流水中可溶性有机碳(DOC)的含量及通量,比较不同森林类型观测结果的差异,并分析降雨对实验结果的影响。结果表明:米槠人工幼林单次产流量是米槠次生林的1.5—19.0倍,观测期间总径流量为5.9倍;米槠人促幼林单次径流量和总径流量均与米槠次生林无显著差异(P0.05)。观测期间米槠次生林、人工幼林、人促幼林径流水DOC浓度值范围为5.9—18.4 mg/L,4.3—13.5 mg/L和3.2—9.9 mg/L,米槠次生林径流水浓度均值(12.6 mg/L)分别是米槠人促幼林(7.6 mg/L)和米槠人工幼林(5.3 mg/L)的1.6和2.4倍。回归分析表明,径流水中DOC浓度与降雨前土壤含水率呈显著相关;降雨前土壤含水率20.8%是一个临界值,含水率低于20.8%时,径流水DOC浓度与降雨前含水率呈显著正相关(P0.05);高于20.8%时,径流水DOC浓度与降雨前土壤含水率呈显著负相关(P0.05)。米槠人工幼林地表径流DOC输出通量是米槠次生林的0.7—5.4倍,观测期间总输出通量为2.1倍;米槠人促林DOC单次通量和观测期间总通量均与米槠次生林差异不显著(P0.05)。三种森林类型DOC输出通量均与降雨量呈显著相关(P0.05)。可见,米槠次生林转变成米槠人工幼林后DOC输出浓度降低,但径流量显著增加,导致DOC输出通量增加;而转变成米槠人促幼林后DOC输出浓度也降低,但径流量并未增加,因而并未增加DOC输出通量。     

Age of arboreous Tamarix austromongolica and its growth response to environment in Tongde County of Qinghai,China

Aims The objectives were to identify the age of the arboreous Tamarix austromongolica in the flood plain area of the Qinghai Plateau and clarify the response patterns of T. austromongolica’s growth to the environmental factors. We focused on social issues about whether the T. austromongolica should be protected and how to protect in the reservoir area of a hydropower station. Methods In this study, arboreous T. austromongolica in both reservoir submerged and non-submerged areas were sampled and measured based on the dendrochronology method. The ages were estimated based on the geometrical characteristics of the pith and the identified age of the inner ring. The correlation and response analysis showed the relationship between T. austromongolica’s growth and environmental factors. Important findings We accurately determined the age and historical growth dynamics of the T. austromongolica with large diameter at breast height (DBH). The results showed a special accretion phenomenon in arboreous T. austromongolica, which accelerated the DBH increasing, i.e. no direct relationship existed between the plants’ DBH and ages of the individuals. Radial growth of T. austromongolica, increased rapidly in the 1970s and 1980s and began to stabilize in the late 1980s, and mainly responded to the runoff in July and August of the Yellow River. Increasing runoff would promote the radial growth of T. austromongolica. The growth of the immaturate plant showed significant negative correlation with the wind speed in the growing season. The results will be of theoretical significance to the formation of the special morphology of the T. austromongolica, and will provide scientific practical guidance in designing the protection schemes.     

Misapplication of generic hazard-classification schemes for versatile,sustainable building materials: Copper as an example

Decisions regarding the use of building materials are being made based solely on the hazards of chemicals, without conducting risk assessments that account for realistic potential exposures and effects. We present copper as an example of a versatile, sustainable building material for which hazard classification has been misapplied. As a result, copper has been “blacklisted” for use as an exterior building material. However, its purported human health effects are not relevant for exposure to exterior building materials; furthermore, the potential environmental effects to aquatic life are not considered in appropriate contexts. We recommend evaluating risks of copper in runoff water at the point in temporal, chemical, and physical spaces at which organisms of concern will be exposed, instead of evaluating copper concentrations at the point of runoff from copper roofs, gutters, etc. Instead of banning a building material, appropriate institutional controls and/or best management practices should be required to control the release of related substances, if needed. In the absence of risk and/or life cycle assessments, architects and builders might choose regrettable substitutions in which materials posing unknown but potentially higher risks will replace more completely characterized materials that have lower risk in a given application.     

基于景观尺度过程模型的长白山地表径流量时空变化特征的模拟

运用已建立的景观尺度生态系统生产力过程模型EPPML对长白山自然保护区地表径流量的季节动态和空间分布特征进行了模拟,对其与环境因子间的相互关系进行了分析．模拟结果表明,长白山自然保护区地表径流量的季节进程表现出明显的三峰型,6月和9月出现低谷,8月达最大(2．58mm·d^-1),与土壤含水量的季节变化趋势十分相似．1995年地表径流量的模拟值平均为0．203m·年^-l,空间分布随海拔升高呈现明显增加的趋势,最高为高山流砾滩(0．619m·年^-1),最低为阔叶红松林(0．081m·年^-1)．年地表径流量与叶面积指数(LAI)呈极显著负相关指数关系(R^2＝0．857)．年地表径流量与气温和总辐射呈负相关关系(R^2分别为0．965和0．836),与降水量、相对湿度和风速呈正相关关系(R^2均大于0．950),还与土壤特性密切相关。     

河网地区小城镇街尘的粒径分布与多环芳烃污染

街尘是重要的环境介质,其携带的污染物在城镇化过程中对河网地区的水环境构成了一定的威胁。以杭嘉湖平原河网地区饮用水水源河流上游典型小城镇的街尘为研究对象,对街尘、河道沉积物、地表径流以及降雨前后地表水中的多环芳烃进行测定。在对不同粒径街尘中多环芳烃浓度的测定中发现,粒径为<63、125-63、250-125和900-250 μm街尘中多环芳烃的平均含量分别为7261、5835、4660和2909μg/kg。小粒径的街尘颗粒含有较高的多环芳烃浓度,较小的密度,并且较难清扫,造成了小粒径街尘易被雨水冲刷随地表径流进入河网水体。在对两场降雨的地表径流中多环芳烃检测发现,颗粒态的多环芳烃分别占总浓度的95%和94%。地表径流过程增加了受纳水体中多环芳烃浓度的43%-62%,其中超过50%的增加表现为颗粒态。在对不同河段沉积物、地表径流中颗粒物和不同粒径街尘中多环芳烃浓度的风险评价中发现,小粒径街尘和地表径流中颗粒物中多环芳烃的浓度相接近并具有较高的生态风险,城镇段河道沉积物较次之。由于河网地区的特殊的水文条件和景观空间格局特征,地表径流沉积物在进入河网水体后易原位沉积,造成了河道沉积物城镇段有较高的多环芳烃浓度。     

GIS-based distributed model for simulating runoff and sediment load in the Malian River Basin

GIS-based modeling is an effective approach for reflecting spatially-varied complexities in watershed systems. In this study, a GIS-aided distributive hydrological model was developed to simulate runoff and sediment transport in a loess-plateau context with semi-arid climate, sparse vegetation, and serious soil erosion. The model was then applied to a case study in the Malian River Basin, which is one of the largest catchments in the middle reach of the Yellow River. Based on the GIS technique, the DEM of the study basin was successfully used to delineate the stream network and extract information of catchment characteristics. The results show satisfactory accuracy for runoff simulation. Especially, the integrated soil-erosion and hydrological models can be used for simulating both runoff and sediment loads, which provide a useful decision-support tool for water resources management and pollution control. This study is an attempt to develop a distributed rainfall-runoff model for river basins in the loess plateau region. The developed model can also be extended to larger basins. Further works of field survey and investigation would be helpful for better calibrating critical parameters and thus improving performance of the developed model.     

长期施磷对黄壤旱地磷库变化及地表径流中磷浓度的影响

对贵州黄壤旱地进行采样以及盆栽试验,探索黄壤旱地磷库的变化及其对地表径流磷量的影响。结果表明,长期施磷后黄壤旱地无机磷占全磷的比例逐渐增高,Al-P、Fc-P和Ca-P积累的顺序为Fe-P>Al-P>Ca-P。长期施磷后黄壤旱地的有效磷和藻类可利用的总磷也不断积累,高磷（Olsen-P>25mg·kg^-1)旱地藻类可利用的总磷与Al-P、Fe-P和Ca-P的相关系数分别为0.859、0.903和0.650,Fc-P对藻类可利用磷量的影响起着最重要的作用。在模拟雨强为63.2mm·h^-1下,降雨30min后,低磷黄壤旱地（Olsen-P为4.62-15.9mg·kg^-1)径流中磷酸根磷含量仅为2.81-4.17μg·L^-1,生物有效性磷含量为0.723-0.876mg·L^-1;高磷黄壤旱地（Olsen-P)为29.4-59.2mg·kg^-1)径流中磷酸根磷含量达到0.026-0.714mg·L^-1,生物有效性磷含量增加到0.996-1.281mg·L^-1;高磷黄壤旱地地表径流磷量能加速水体富营养化的产生。     

Phosphorus retention in lab and field-scale subsurface-flow wetlands treating plant nursery runoff

Constructed wetland systems built to handle nutrient contaminants are often efficient at removing nitrogen, but ineffective at reducing phosphorus (P) loads. Incorporating a clay-based substrate can enhance P removal in subsurface-flow constructed wetland systems. We evaluated the potential of crushed brick, a recycled building product, and two particle sizes of a palygorskite–bentonite industrial mineral aggregate (calcined clay) to sorb P from simulated nutrient-rich plant nursery effluent. The three substrates were screened for P sorbing behavior using sorption, desorption, and equilibration experiments. We selected one substrate to evaluate in an 8-month field trial to compare field sorption capacity with laboratory sorption capacity. In the laboratory, coarse calcined clay average sorption capacity was 497 mg kg⁻¹ and it sorbed the highest percentage of P supplied (76%), except at exposure concentrations >100 mg L⁻¹ where the increased surface area of fine calcined clay augmented its P sorption capacity. Subsurface-flow mesocosms were filled with coarse calcined clay and exposed to a four and seven day hydraulic retention time treatment. Phosphorus export was reduced by 60 to 74% for both treatments until substrate P-binding sites began to saturate during month seven. During the eight month experiment, the four and seven day treatments fixed 1273 ± 22 mg kg⁻¹ P and 937 ± 16 mg kg⁻¹ P, respectively. Sequential extractions of the P saturated clay indicated that P could desorb slowly over time from various pools within the calcined clay; thus, if the calcined clay were recycled as a soil amendment, most P released would be slowly available for plant uptake and use. This study demonstrated the viability of using coarse calcined clay as a root bed substrate in subsurface-flow treatment wetlands remediating phosphorus from plant nursery runoff.     

1967—2006年太子河流域径流系数的变化特征

利用太子河流域6个主要支流（海城河、南沙河、北沙河、兰河、细河、太子河南支）1967—2006年日均降水和径流资料,分析了各支流径流系数的变化趋势及其与降水的关系.结果表明：1967—2006年,位于高山丘陵区的太子河南支的年均径流系数较大,而人类活动影响较多的海城河流域的年均径流系数较小;除南沙河的年径流系数总体呈上升趋势外,其余各条支流的年径流系数均呈下降趋势,以南支和兰河的下降趋势尤为明显;除细河流域的年径流系数没有发生突变外,其余各条支流的年径流系数都发生了突变,且突变出现的年份各不相同;年降水量对年径流系数的影响极显著.