巢湖水体悬浮物含量与光谱反射率的关系

利用高光谱地物光谱仪在巢湖进行了反射光谱测量和同步水质采样分析，在分析巢湖水体反射光谱特征的基础上，分别研究了悬浮物浓度与水体光谱反射率和光谱反射率的一阶微分之间的关系，结果表明在近红外波段范围，单波段反射率和一阶微分光谱反射率都与悬浮物的浓度有较好的相关性，而且利用微分光谱估算内陆水体悬浮物浓度有较大潜力。     

上海市蔬菜地土壤硝态氮状况研究

以上海市郊不同管理方式下菜地表层土壤采样测定土壤硝态氮含量为基础,并以水稻土等土壤作为对照,以期了解上海蔬菜地土壤硝态氮的现状,为菜地的合理施肥提出科学依据。结果表明,由于管理方式不同,土壤的硝态氮的NO3--N质量分数差异明显。大棚蔬菜地土壤中NO3--N明显高于其它其他用地管理方式下的土壤,依次为:w(大棚蔬菜地)>w(露天蔬菜地)>w(传统自留地),而且土壤硝态氮的积累是全剖面性的,而非仅在表层,如在80~100cm土层,大棚土壤硝态氮也为农田的好几倍。而且,大棚蔬菜地土壤盐渍化明显,主要特点之一是硝态氮积累,盐分高的土壤一般硝态氮也高。此外,长期大量的N肥投入引起了土壤酸化。土壤pH与土壤NO3--N质量分数呈线性负相关,经统计检验相关性达极显著水平。     

镉对稻田土壤典型微生物种的胁迫生理毒性

以水稻田土壤中典型的单种微生物为实验材料,采用纯培养方法,从个体水平上全面探讨了重金属镉胁迫对稻田土壤典型微生物的的生长、活性以及生化过程的生理毒性影响。研究表明:不同微生物纯培养对镉胁迫的敏感程度不同,G 较G-对Cd2 更为敏感,表现为世代时间缩短,最高菌浓度下降。固氮菌对Cd2 非常敏感,当Cd2 质量浓度为0.2mg·L-1时即完全抑制菌体增殖。同时,外源镉强烈的抑制作为稻田土壤中功能微生物的厌氧固氮菌及产甲烷细菌的生物活性,各菌种镉胁迫下细菌细胞内可溶性蛋白、还原糖、核酸质量浓度都在低质量浓度镉胁迫时有所增加;随着镉质量浓度的增加,细菌细胞内各种物质的质量浓度开始减小,以减慢细胞代谢速度,增强对镉胁迫的适应力;各种物质的质量浓度变化趋势为可溶性蛋白>还原糖>核酸,R.eutrophaDKC1细胞内含物质量浓度基本保持稳定。结果可在一定程度上说明镉对微生物的毒性效应,且能在早期较灵敏地指示污染的影响,作为稻田土壤环境受到污染胁迫的细胞生化指标具有一定可行性。     

农杆菌介导将高赖氨酸蛋白基因导入谷秆两用水稻

采用农杆菌介导法将高赖氨酸蛋白基因导入到谷秆两用水稻中，GUS组织化学染色、PCR扩增、Southem blot分析表明，该基因已经整合到水稻基因组中，测定9株转基因水稻叶片赖氨酸含量，大部分植株有明显的提高，最高幅度达到了22．71％，图6参15     

盐碱土壤基质人工湿地对低浓度氮磷废水的净化效果

采用实验室模拟研究了以盐碱土壤为基质的不同湿地植物人工湿地系统以及对水中低质量浓度氮和磷的去除效率。实验表明，芦苇系统、香蒲系统、车钱草系统和无植物系统均对水中低质量浓度的N具有净化效果。3种植物系统相比，香蒲系统的净化效果较其他二者较佳，芦苇系统与车钱草的净化效果相当；同时实验也表明4种湿地系统对低质量浓度的P不具有净化效果，随着水力停留时间的增加，系统中的P质量浓度反而会有所增加。     

外加镍在土壤中的形态与再分配

镍处理土壤经室内培养12周后,采用连续提取技术对试验土壤中镍的形态与再分配方式进行了研究。研究结果表明,外加的水溶性镍进入土壤后的主要存在形态与添加的剂量有关:低剂量时,以铁锰氧化态为主,这一形态在100mg·kg-1处理土壤中占比例最大,达到31.6%;高剂量时,以交换态为主,这一形态在1600mg·kg-1处理土壤中占比例最大,达到48.4%。随着镍添加剂量由0(对照)增加到1600mg·kg-1,再分配系数逐渐由1.00增大到30.65;金属结合强度系数则由0.90减小至0.25,也反映出进入土壤中镍的剂量较大时,镍是以不稳定的形态占优。试验结果也证实了土壤具有减小镍的环境危害的作用,但这种缓冲能力是有限的。随着时间的推移,镍的形态会继续发生变化,但这一转化过程是缓慢的。因此,一旦土壤发生重金属污染,其对土壤环境的影响将是长期的。     

芜湖市郊土壤污染对土壤动物群落结构的影响

研究表明，芜湖市郊农田土壤动物群落的组成与数量随污染程度的加重而减少，土壤动物密度也呈同样的变化趋势，特别是中小型土壤动物，优势类群数量发生较大消长，常见类群和稀有类群的组成逐渐减少．多样性指数H与重金属污染程度之间关系因受到季节的影响而变得复杂：冬季和初夏污染较重样地优势类群数量减少，群落均匀性指数E增加而优势度指数C减小，多样性指数H较高；而春季处于过渡阶段，某些类群(如螨类)数量爆发，C增高，H较小．土壤动物群落密度一类群指数DG随污染加重而减小．受到重金属污染的农田土壤动物的表聚性减弱，甚至出现逆分布现象．图1表4参15     

Changes of Soil Microbiological Properties Caused by Land Use Changing From Rice–Wheat Rotation to Vegetable Cultivation

A survey was done recently in Jiaxing city of Zhejiang Province in the Yangtze River Delta to compare the differences of soil microbiological properties among paddy soils with different land use including continuous open-field vegetable cultivation (OFVC), plastic-greenhouse vegetable cultivation (PGVC) and traditional rice–wheat rotation (RWR). The soil types included are percolating, permeable and waterlogged paddy soils. The results indicate that the microbial flora was markedly changed as the land use changed for all the three soil types. In continuous vegetable cultivation soils, especially in PGVC soils, the bacteria amounts decreased dramatically, but the fungal and actinomyce amounts increased as compared with RWR soils. The dehydrogenase activities decreased significantly in vegetable soils, especially in PGVC soils as compared with RWR soils. The microbial biomass C and the total phospholipid contents (TPL) in vegetable cultivation soil greatly decreased as compared with RWR soils. Biolog analysis indicated that the kinds of carbon sources that could be metabolized by native microbes in PGVC soils greatly decreased as compared with OFVC soils and RWR soils, revealing that microbial diversity had decreased since land use change. The activities of some soil enzymes including urease, invertase and phosphase were all lower in OFVC soils than those in RWR soils, and those in PGVC soils were the lowest. The degradation of microbiological activities in continuous vegetable cultivation soils, especially in PGVC soils, as compared with RWR soils might have been caused by soil acidification and accumulation of salts due to overuse of both organic and inorganic fertilizers in vegetable cultivation.     

磷肥施用量对缺锌土壤上水稻生长的影响

磷肥施用量对缺锌土壤上水稻生长的影响李延，潘伟彬（福建农业大学土化系，福州３５０００２）（闽西职业大学，龙岩３６４０２１）ＥｆｆｅｃｔｏｆＰｈｏｓｐｈａｔｉｃＦｅｒｔｉｌｉｚｅｒｏｎＧｒｏｗｔｈｏｆＲｉｃｅｏｎＺｉｎｃＤｅｆｉｃｉｅｎｔＳｏｉｌ￥Ｌｉ...     

Soil Lead at Elementary Public Schools: Comparison Between School Properties and Residential Neighbourhoods of New Orleans

Soil studies, conducted in Maryland, Minnesota and Louisiana, have described the urban pattern of lead contamination. They have shown that the highest amounts of lead cluster within the interior of the largest cities. The results of the New Orleans urban patterns of distribution of soil lead provided the basis for further study. The hypothesis was tested that elementary school properties have the same pattern of soil lead contamination as their neighbouring residential communities. Thirty New Orleans Public Elementary Schools were selected for this study. Surface samples (2.5cm or 1 inch depth) were collected from playgrounds and next to entrances of each school. Results showed that soil lead on school properties follows the same relative contamination patterns (pvalue10^–5) as soil lead on residential properties of neighbouring communities. Schools however, have significantly lower lead contamination than the neighbouring residential properties. Innercity school properties present a higher risk of soil lead exposure than mid and outercity schools. Soils next to innercity school entrances showed the highest lead, with 18.5% having concentrations over 400gg^–1. Systematic landscaping around the school entrances would significantly reduce the hazard from lead dust contaminated soils.