基于神经网络模型的中国表层土壤有机质空间分布模拟方法

基于全国第二次土壤普查得到的6 241个典型土壤剖面数据,采用主成分分析方法和径向基函数神经网络模型建立不同植被类型—土纲单元内土壤有机质与气候、地形和植被等环境因子间的非线性关系,模拟全国表层土壤有机质的空间分析格局。结果表明,该模型具有较准确的预测能力,性能指数达到1.94。与普通克里格法、反比距离法和多元回归模型相比,神经网络模型对621个验证点模拟结果与实测值的相关系数为0.799,分别提高了0.265、0.181和0.120,平均绝对误差分别降低了4.25、4.43和2.34 g/kg,平均相对误差分别降低了30.16%、32.66%和5.93%,均方根误差则分别降低了8.61、8.24和6.24 g/kg;从模拟结果图来看,神经网络模型能够提供更多的细节信息。该方法为大尺度土壤性质空间分布模拟提供了有益的参考。     

Isozyme analysis of spotted halibut Verasper variegatus temminck et schlegel

To investigate the tissue-specificities of isozymes and the genetic structure of wild spotted halibut (Verasper variegates) population, horizontal starch gel electrophoresis was performed on 45 individuals collected in part of the Yellow Sea. The performances of 17 isozymes in 8 kinds of tissues or organs were screened preliminarily in a TC-7.0 buffer system. The results showed that the screened isozymes displayed remarkable tissue-specificities. Finally, 14 enzymes (AAT, ADH, EST, GPI, G3PDH, IDHP, LAP, LDH, MDH, MPI, PGDH, PGM, SDH and SOD) and 4 kinds of tissues (eye, skeleton muscle, liver and heart) were selected for genetic analysis. Fourteen isozymes are encoded by 20 loci, and 9 of them are polymorphic. The polymorphic loci are AAT-1*. GPI-2* G3PDH*, IDHP-1*, LDH*, MPI*, PGM-1*. PGM-2* and SDH*, and the proportion of polymorphic loci is 0.4500 (P0.99). The mean values of observed and expected heterozygosities are 0.027 8 and 0.026 5, respectively and the average effective number of alleles is 1.067 5.     

区域可持续发展集成模型的分析与应用研究——以黄河三角洲地区为例

 本文在总结国内、外可持续发展指标体系的基础上,按照信息的综合水平将黄河三角洲可持续发展指标体系区分为I级指标体系和II级指标体系,其中I级指标体系对应数据库,II级指标体系对应模型库。在分析多目标决策模型、风险决策模型和系统动力学模型等综合模型优、缺点的基础上,提出了黄河三角洲可持续发展集成模型的研究框架。总结了近几年来黄河三角洲可持续发展集成模型的研究进展和正在进行的研究工作,讨论了进一步需要研究的内容     

Partial Sequence Analysis of Mitochondrial COI Gene of the Chinese Shrimp, Fenneropenaeus Chinensis

Eight hundred and thirty eight base pair fragment of mitochondrial COI gene of wild and cultured populations (CP1, CP4, CP5 and CP6) of Fenneropenaeus chinensis was amplified and sequenced. The A, T, G and C contents of the sequence were 235bp (28.0% ),.307bp (36.6%), 138bp (16.5%) and 158bp (18.9%), respectively. Furthermore, 556bp fragment of the sequence was used to discuss the phylogenetic relationship among 14 Penaeidae species using Alpheus armillatus as the outgroup. From the molecular phylogenetic tree constructed by neighbor-joining method, we obtained three large shrimp groups: Farfantepenaeus, Litopenaeus and Fenneropenaeus group. The results also indicated that there were a closer genetic relationships between F. aztecus and F. paulensis, L. schmitti and L. setiferus, F. indicus and F. merguiensis, and the genus Farfantepenaeus was closer to Litopenaeus.     

Phenology shift from 1989 to 2008 on the Tibetan Plateau: an analysis with a process-based soil physical model and remote sensing data

Phenology is critical to ecosystem carbon quantification, and yet has not been well modeled considering both aboveground and belowground environmental variables. This is especially true for alpine and pan-arctic regions where soil physical conditions play a significant role in determining the timing of phenology. Here we examine how the spatiotemporal pattern of satellite-derived phenology is related to soil physical conditions simulated with a soil physical model on the Tibetan Plateau for the period 1989–2008. Our results show that spatial patterns and temporal trends of phenology are parallel with the corresponding soil physical conditions for different study periods. On average, 1 °C increase in soil temperature advances the start of growing season (SOS) by 4.6 to 9.9 days among different vegetation types, and postpones the end of growing season (EOS) by 7.3 to 10.5 days. Soil wetting meditates such trends, especially in areas where warming effect is significant. Soil thermal thresholds for SOS and EOS, defined as the daily mean soil temperatures corresponding to the phenological metrics, are spatially clustered, and are closely correlated with mean seasonal temperatures in Spring and Autumn, respectively. This study highlights the importance and feasibility of incorporating spatially explicit soil temperature and moisture information, instead of air temperature and precipitation, into phenology models so as to improve carbon modeling. The method proposed and empirical relations established between phenology and soil physical conditions for Alpine ecosystems on the Tibetan plateau could also be applicable for other cold regions.     

兖州市采煤塌陷地生态治理模式探讨

介绍了兖州市采煤塌陷地综合治理的几种传统方法及生态治理模式。结合兖州市采煤塌陷地综合治理实际情况,通过传统治理模式与生态治理模式在经济、社会、环境方面的效益对比分析,提出了采煤塌陷地以生态治理为主导的观点。     

中国气温与降水的时空变化趋势分析

如何对离散分布的气象台站观测数据进行高精度曲面模拟,为生态系统及服务功能时空变化趋势模拟及其综合评估提供高质量、高分辨率的空间气候数据,以满足栅格层次上的生态系统过程模型、生态系统格局模型及生态系统综合评估模型的参数需求,一直是存于生态学界的难点问题.在对全国1964一2007年的752个气象台站长期观测的气温和降水数...     

Preliminary Study on the Water Drag of Schlegel's Black Rockfish Sebastes schlegeli

1　Introduction　FishcageculturesystemhasbeenwidelyusedinmaricultureindustryinChina .Indesigningthecagesystem ,thewaterdragactingonit,includingthatonculturedfish ,shouldbetakenintoaccount.Avarietyofmethodshavebeenusedtodeterminethewaterdragofanimalsrangin…     

逐次最小二乘在高精度曲面建模方法（HASM）中的应用

从高精度曲面建模方法（HASM）曲面方程出发,结合数据平差理论,建立了基于独立单元的计算模型,并且采用逐次最小二乘法对计算方程进行分组求解。对HASM-AD和几种经典方法的精度进行了交叉验证,结果表明,该算法模拟误差的均方根差远小于其他空间插值方法。     

Structure of mitochondrial DNA control region of Pholis fangi and its phylogenetic implication

In this study, the entire mitochondrial DNA （mtDNA） control region （CR） of Pholis fangi was amplified via polymerase chain reaction followed by direct sequencing. The length of the mtDNA CR consensus sequence of P. fangi was 853 bp in length. In accordance with the recognition sites as were previously reported in fish species, the mtDNA CR sequence of P. fangi can be divided into 3 domains, i.e., the extended terminal associated sequence （ETAS）, the central conserved sequence block （CSB）, and the CSB domain. In addition, the following structures were identified in the mtDNA CR sequence of P. fangi：2 ETASs in the ETAS domain （TAS and cTAS）, 6 CSBs in the central CSB domain （CSB-F to CSB-A）, and 3 CSBs in the CSB domain （CSB-1 to CSB-3）. These demonstrated that the structure of the mtDNA CR of P. fangi was substantially different from those of most other fish species. The mtDNA CR sequence of P. fangi contained one conserved region from 656 bp to 815 bp. Similar to most other fish species, P. fangi has no tandem repeat sequences in its mtDNA CR sequence. Phylogenetic analysis based on the complete mtDNA CR sequences showed that there were no genetic differences within P. fangi populations of the same geographical origin and between P. fangi populations of different geographical origins.