安徽省沿淮地区梅雨特征及其时空分布分析

论文在探索安徽沿淮地区梅雨期(包括入梅期、出梅期和梅雨长度)、梅雨量和梅雨强度(包括梅期平均日雨量、雨量梅年比、梅期暴雨日数和梅雨强度指数)特征的基础上,着重分析了安徽沿淮地区梅雨期、梅雨量和梅雨强度的年际变化以及安徽沿淮一带11站梅期雨量和雨强地域分布的差异性。结果发现:①安徽沿淮地区多年平均梅雨期为24d(6月16日入梅, 7月10日出梅),梅雨量为221.9mm,梅期日雨量为8.6mm,雨量梅年比为22.3%,暴雨日数为1.3d,梅雨强度指数为4.0;②沿淮历年梅雨特征量均呈明显的波动趋势;③沿淮梅期雨量和雨强年际变化的平均波动周期约为9年,但随年代推移具有振幅减小和频率加快的特点;④安徽沿淮自西向东各站梅期雨量和雨强均呈"升-降-升"S型分布趋势。这些发现对于沿淮各地气候研究和天气预报具有重要的参考价值。     

Ecosystem health assessment of urban rivers and lakes-Case study of "the six lakes" in Beijing,China

The assessment of the ecosystem health of urban rivers and lakes is the scientific basis for their management and ecological restoration. This study developed a three-level indicator system for its assessment. The results indicated that: Zhonghai and Nanhai are in the state of transition from unhealthy to critical state and all the other lakes are in unhealthy states. Water environmental quality, structure and function of the aquatic ecosystem, and the structure of waterfront areas were the constraints. Nanhai was ranked as poor and the others were all ranked as very poor. However, the ecological environment of Zhonghai and Nanhai were better than the others, the sums of the degree of membership to the healthy state and critical state were all close to 0.6. and the restorations of these lakes were moderate. The sums of the degree of membership to the healthy state and critical state of the other lakes were under 0.3, as it was difficult to restore these lakes. Some suggestions on scientific management and ecological restoration of the six lakes were proposed: ①To control non-point pollution and to improve the water quality of six lakes and the water entering into these lakes; ②To improve the hydrological conditions of six lakes; ③To rehabilitate the aquatic ecosystem and waterfront areas. __________ Translated from Acta Ecologica Sinica, 2005, 25(11): 3019–3027[译自: 生态学报]     

常熟市农业和农村污染的优先控制区域识别

农业和农村污染发生的广域性、分散性和随机性等特征,使得农村污染治理难以抓住重点.在乡镇级单元尺度上,采用清单分析法,核算江苏省常熟市农田种植(化学肥料施用和作物秸秆遗弃)、畜禽养殖、水产养殖、农村生活(生活污水和人粪尿、生活垃圾)共4类6种农业和农村污染源的化学需氧量(COD)、全氮(TN)、全磷(TP)排放量和排放强度,采用聚类分析法,通过敏感性评价识别出农业和农村污染的优先控制区域和优先控制污染源,从而使得农业和农村污染控制与管理措施更具针对性.结果表明,2007年常熟市农业和农村污染源COD、TN和TP的排放量分别为5496.07、4161.03、647.54t.a-1,COD、TN和TP的排放强度分别为48.84、36.98、5.75kg.hm-2.COD的主要污染源是农村生活和水产养殖,贡献率在75%以上,TN和TP的主要污染源是农田种植和水产养殖,贡献率在80%以上.敏感性评价识别出古里镇和沙家浜镇是常熟市农业和农村污染的优先控制区域,农田种植和水产养殖是优先控制区域内要优先控制的污染源.     

物元模型在综合评价旅游环境承载力中的应用

为了解决评价因素间的不确定性和不相容性问题,采用一种新方法对旅游环境承载力进行综合评价,该方法称为物元分析法。通过建立旅游环境承载力评价标准体系和物元模型来确定一个旅游区的环境承载力状态。以安徽省旅游区为例进行评价,结果表明该方法简单可行。对旅游规划决策和区域旅游业的可持续发展有重要的意义。     

人工湿地在我国北方寒冷地区的应用

概括归纳了人工湿地在北方应用的局限性及其应对措施,提出对湿地保温、改良微生物及其处理过程、合理选择湿地植物和基质、减低负荷等措施,以期使人工湿地在我国北方的应用技术更加成熟,应用区域更加广泛。     

臭氧-生物活性炭对南方河网典型污染物的去除特性

以我国南方河网原水中有机物和季节性溴化物(Br^-)为对象,研究臭氧-生物活性炭(BAC)工艺净化过程中有机物相对分子质量(M_r)分布变化及溴酸盐(BrO^-₃)和消毒副产物(THMs)的形成规律.结果表明,原水中M_r在10³以下的有机物(DOC)约占总量的80%,常规工艺主要表现为对M_r >100×10³有机物的去除,出水DOC去除率为8%、 SUVA(UV₂₅₄/DOC)值下降14%;臭氧-活性炭工艺主要去除10³<M_r<5×10³的有机物,但亲水性小分子有机物抑制生物降解作用,出水DOC去除率仅提高至30%、SUVA值下降31%.当臭氧投加量高于2 mg/Ｌ时,臭氧氧化出水中BrO^-₃增加明显,氧化过程原水中Br^-浓度升高BrO^-₃生成量增大;生物活性炭对BrO^-₃的去除率平均仅为13%,且波动较大.与常规处理相比,臭氧-生物活性炭处理后各类THMs均有减少,总量减少40%;但氯量和Br^-对溴代副产物影响大,主要为CHBr₃生成量增加.     

Soil-profile distribution of carbon and associated properties in no-till along a precipitation gradient in the central Great Plains

No-till (NT) farming is considered as a potential strategy for sequestering C in the soil. Data on soil-profile distribution of C and related soil properties are, however, limited, particularly for semiarid regions. We assessed soil C pool and soil structural properties such as aggregate stability and strength to 1 m soil depth across three long-term (≥21 year) NT and conventional till (CT) experiments along a precipitation gradient in the central Great Plains of the USA. Tillage systems were in continuous winter wheat (Triticum aestivum L.) on a loam at Hutchinson and winter wheat-sorghum [Sorghum bicolor (L.) Moench]-fallow on silt loams at Hays and Tribune, Kansas. Mean annual precipitation was 889 mm for Hutchinson, 580 mm for Hays, and 440 mm for Tribune. Changes in profile distribution of soil properties were affected by differences in precipitations input among the three sites. At Hutchinson, NT had 1.8 times greater SOC pool than CT in the 0-2.5-cm depth, but CT had 1.5 times greater SOC pool in the 5-20-cm. At Hays, NT had 1.4 times greater SOC pool than CT in the 0-2.5-cm depth. Differences in summed SOC pool for the whole soil profile (0-1 m depth) between NT and CT were not significant at any site. The summed SOC pool with depth between NT and CT were only significant above the 5 cm depth at Hutchinson and 2.5 cm depth at Hays. At Hutchinson, NT stored 3.4 Mg ha⁻¹ more SOC than CT above 5 cm depth. At Hays, NT stored 1.35 Mg ha⁻¹ more SOC than CT above 2.5 cm depth. Moreover, NT management increased mean weight diameter of aggregates (MWDA) by 3 to 4 times for the 0-5-cm depth at Hutchinson and by 1.8 times for the 0-2.5-cm depth at Hays. It also reduced air-dry aggregate tensile strength (TS) for the 0-5-cm depth at Hutchinson and Hays and for the 0-2.5-cm depth at Tribune. The TS (r = −0.73) and MWDA (r = 0.81) near the soil surface were more strongly correlated with SOC concentration at Hutchinson than at Hays and Tribune attributed to differences in precipitation input. Results suggested NT impacts on increasing SOC pool and improving soil structural properties decreased with a decrease in precipitation input. Changes in soil properties were larger at Hutchinson (880 mm of precipitation) than at Hays and Tribune (≤580 mm). While NT management did not increase SOC pool over CT for the whole soil profile, the greater near-surface accumulation of SOC in NT than in CT was critical to the improvement in soil structural properties. Overall, differences in precipitation input among soils appeared to be the dominant factor influencing NT impacts on soil-profile distribution of SOC and soil structural properties in this region.     

基于下垫面遥感资料的海河流域水文类型分区划分

以海河流域为研究对象,根据1956—2005年的年降雨量和水面蒸发资料、DEM、土地利用、土壤和植被覆盖遥感图,提取了反映下垫面条件和气候特征的物理因子,并以此作为分区指标,以子流域为划分单元,依据下垫面条件和气候因子的相似性和差异性,采用地理信息系统和多元统计分析的方法,将海河流域内1 399个子流域划分7类水文类型分区(HTR),并分析了各水文类型分区的空间分布特征及产汇流机制。其中HTR1、HTR2和HTR4位于平原地区,土地利用类型以耕地为主,其他水文类型分区位于山区和丘陵区。HTR1耕地面积比例最大;HTR2土壤透水性最差,易产生超渗地表径流;HTR3土壤透水性最好,易产生地下径流和壤中流;HTR4年蒸发量较大,年降雨量较小,气候最干旱;HTR5和HTR6土地利用类型分别以草地和林地为主;HTR7年降雨量较大,年蒸发量较小,气候最湿润。分区成果明确地反映了流域的下垫面情况及气候条件,分区结果与流域的地形地貌非常吻合,也反映了流域水文特征的分布规律。通过分析水文类型分区内典型流域的下垫面和气候情况以及水文特征,阐述了分区结果的准确性及合理性,为海河流域水文特征的研究及水资源评价提供了依据。     

环境约束下的中国八大经济区出口结构优化模拟研究

论文基于2007—2010年中国30个省份区域间投入产出表数据,结合线性规划建立了多区域投入产出优化模型,研究了环境约束下中国八大经济区的出口结构优化。结果表明：2007—2010年需要提高服务业和农业的出口比重,同时降低煤炭开采和洗选业、造纸印刷及文教体育用品制造业、金属冶炼及压延业和电力热力生产供应业的出口比重,通过以上结构调整达到最优出口结构,可以实现在不增加碳、工业二氧化硫和工业废水排放的基础上促使全国GDP分别提高6.84%和8.17%。东北区域、黄河中游区域、长江中游区域、大西南区域和大西北区域需要降低的出口部门较多,且多集中在高能耗高排放产业;东部沿海区域、南部沿海区域、北部沿海区域需要提高的出口部门较多,主要集中在制造业和服务业,2010年东部沿海区域、南部沿海区域和大西北区域的总体出口结构优化度比2007年有所提高。在八大经济区中,东部沿海区域和南部沿海区域由于区位优势,其出口结构整体优化度相对较高,而东北区域则最低。地理区位对于区域出口结构优化具有一定程度的影响。     

不同下垫面土壤凝结水特征及其影响因素

凝结水是干旱区生态系统重要的水分来源。2010年6-7月采用底部连通和不连通的微渗计对塔里木河下游地区胡杨林、柽柳丛和裸地3种典型下垫面土壤凝结水的变化特征、形成时间及其影响因素进行了研究。结果表明:①观测期间研究区裸地土壤凝结水总量最多,其次为柽柳丛的,而胡杨林的最小,其凝结水总量分别为2.60、2.49、1.26 mm,方差分析显示,不同下垫面类型土壤的日均凝结水量之间存在极显著差异(P<0.01);②凝结过程一般从22:00持续到次日8:00,晴天日出后一定时间范围内凝结现象仍继续发生,3种下垫面土壤凝结水量的变化趋势均呈双峰曲线,2:00~4:00左右达到第1个峰值,第2个峰值出现在8:00左右;③连通微渗计产生的凝结水量显著高于不连通微渗计的(t<0.01)。凝结水量主要受气温、大气相对湿度、地温、风速以及下垫面等因素的影响。