1.
Grain-size Distribution and Material Origin of a Paleosol Sequence at Fenghuang Mountain,Chaoyang,Liaoning Province
朝阳凤凰山古土壤序列粒度特征与成因分析
2.
Grain-Size Characteristics and Climatic Changes of a Paleosol Sequence atF enghuang Mountain in Chaoyang,Liaoning Province
辽宁朝阳凤凰山古土壤序列粒度特征与古气候变化
3.
Analgsis on the Magnetic Susceptibility and Its Factors in the Holocene Loess-Paleosol Profile on thd Upper Reaches of Weihe and Paleoenvironment Evolution;
渭河上游全新世黄土—古土壤序列磁化率及影响因素分析
4.
Distribution of trace elements in Holocene loess-paleosol sequence and environmental change in the upper reaches of Jinghe River
泾河上游全新世黄土-古土壤序列微量元素分布特征及环境变化
5.
The Natural Dose-rate of Holocene Loess-soil Sequences in Eastern Gansu Plateau in China
陇东高原全新世黄土古土壤沉积序列辐射环境研究
6.
Ecological Series of Soil Animals in Zuojia Natural Reserve;
左家自然保护区土壤动物生态序列研究
7.
Soil Respiration and Total Belowground Carbon Allocation Along a Chinese Fir Chronosequence
杉木林年龄序列土壤呼吸与地下碳分配
8.
16S rDNA Sequence Analysis of a Agar Degeneration Bacterium QM64 Separated from Soil
一株土壤琼胶降解菌QM64的16S rDNA序列分析
9.
Speciation Analysis of Calcium and Magnesium in Soil and Their Extraction Sequence
土壤中钙、镁的形态分析及提取序列的研究
10.
Network Model Reconstruction of Soil Pore Based on the Serial Digital Images
基于序列图像的土壤孔隙网络模型构建
11.
The number of loess and paleosol units in Quaternary sequences of the Middle Danubian Basin is often closely related to the geological and geomorphological position of the sediment series.
文章叙述了多瑙河中游盆地的第四系黄土与古土壤层序。
12.
Study on the High-Resolution Sequence of Luminescence Dating in the Heilu Soil of Luochuan;
洛川全新世土壤沉积剖面高分辨率年代序列研究
13.
Soil Nutrient Dynamics in Sequencially Aged Eucalyptus Plantations in Mountainous Region of Southern Fujian,China
闽南山区连续年龄序列桉树人工林土壤养分动态
14.
Isolation,identification,and sequence analysis of rDNA-ITS of Pythium species sampled from rhizosphere soil of corn
玉米根围土壤中腐霉菌的分离鉴定及核糖体DNA-ITS序列分析
15.
The spatial distribution and influencing factors of soil trace elements of eucalyptus plantation in continuous age sequences
连续年龄序列桉树人工林土壤微量元素含量及其影响因素
16.
The order of Df (desorption factor) value was: yellowish red soil>silt-loamy soil>kaoline>perlite>paddy soil (loamy clay) >kieselguhr.
解吸因数的大小排列顺序为:黄红壤、粉泥土、高岭土、珍珠岩、青紫泥、硅藻土。
17.
soil erodibility value nomograph
土壤可蚀性值列线图
18.
THE PALE0CLIMATE SIGN1FICANCE RECORDED BY THE COMPACT-CORRECTED CLIMATE PROXY OF LATE TERTIARY EOLIAN SEQUENCE ON THE CHINESE LOESS PLATEAU
晚第三纪以来黄土高原风积序列的压实校正及其古气候意义