土动力学情况简介

<正> 土动力学(Soil dynamics)是土力学的一个分支。它研究动力作用(包括爆炸、地震和动力机械基础振动三个大方面)如何影响周围的土质、对邻近的结构物产生什么样的效应以及如何设计这种结构物来抵抗这种效应等。广义的说,它牵涉到土体中应力和变形随时间快速变化的问题。

土壤中PAHs的光催化降解动力学及机制研究

本文以土壤为介质，以三环的菲（Phe）、四环的芘（Pyr）和五环的苯并[a]芘（BaP）为目标污染物，研究了紫外灯照射下土壤中多环芳烃（PAHs）的降解，并以半导体纳米TiO2和Fe2O3为催化剂研究了土壤中PAHs的催化降解，对光降解及光催化降解的动力学进行了研究，在室内条件下考察了土壤条件和环境因子对光降解及光催化降解PAHs的影响；研究了太阳光照条件下土壤pH值对光降解和催化降解的影响和腐殖酸对光降解的影响；初步探讨了纳米TiO2催化光降解土壤中PAHs的机制。 研究结果表明：土壤中PAHs的紫外光降解符合一级动力学模型，土壤中PAHs光降解与土壤厚度呈显著负相关，土壤粒径对紫外光解PAHs有显著影响，温度从20 ℃升高到30 ℃，光解速率逐渐增加，在PAHs污染土壤的光降解中腐殖酸起敏化作用，随着紫外辐射强度的增加，光降解速率加快。 纳米TiO2和Fe2O3均能促进土壤中PAHs的紫外光降解，PAHs光催化降解符合一级动力学模型，在酸性和碱性土壤条件下，光催化降解PAHs的速率均高于中性，在不同光质条件下，TiO2 、Fe2O3催化光降解PAHs的速率发生变化，随着紫外辐射强度的增加，光催化降解速率常数增加，半衰期减少；腐殖酸促进TiO2 、Fe2O3催化土壤中PAHs的光降解，腐殖酸在这个过程中起着敏化作用。 在太阳光照射下酸性和碱性土壤中PAHs的降解快于中性，PAHs污染土壤中在加入腐殖酸后光降解速率加快，在酸性条件下催化降解最快，在碱性和中性条件下相差不大。 土壤中PAHs存在着PAH的光致电离、电子向O2的转移的两种降解途径；在有催化剂TiO2条件下，由于催化剂在光照后形成的电子-空穴能够氧化还原污染物，PAH的光致电离、电子向O2的转移的引起的降解，共同促进了土壤中PAHs的光催化降解。

Natural 13C abundance as a tracer for studies of soil organic matter dynamics

A method for measuring the long- and medium-term turnover of soil organic matter is described. Its principle is based on the variations of 13C natural isotope abundance induced by the repeated cultivations of a plant with a high 13C/12C ratio (C4 photosynthetic pathway) on a soil which has never carried any such plant. The 13C/12C ratio in soil organic matter being about equal to the 13C/12C ratio of plant materials from which it is derived, changing the 13C content of the organic inputs to the soil (by altering vegetation from C3 type into C4 type) is equivalent to a true labelling in situ of the organic matter. Two cases of continuous corn cultivation (Zea mays: δ13C = −12%.) on soils whose initial organic matter average δ13C is −26%. were studied. The quantity of organic carbon originating from corn (that is the quantity which had turned-over since the beginning of continuous cultivation) was estimated using the 13C natural abundance data. After 13 yr, 22% of total organic carbon had turned-over, in the system studied. Particle size fractions coarser than 50μm on the one hand, and finer than 2μm on the other. contained the youngest organic matters. The turnover rate of silt-sized fractions was slower