pH和有机酸对氟溶出砖红壤中铝离子的影响

研究砖红壤对F-的吸附反应尤其是随后Al3+的释放过程,有助于增进对土壤酸化过程及其环境影响的理解. 在初步揭示出F-吸附反应以及Al3+释放反应的动力学特征基础上,重点考察了pH和有机酸对上述反应的影响. 结果表明:土壤对F-的吸附反应十分迅速,2 min内吸附量即可达到24 h内总吸附量95%,而土壤中不同含铝矿物的溶解度差异使Al3+的释放过程在前15 min十分迅速,释放量可达24 h内总释放量的80%,随后则逐渐减缓. 降低反应体系pH可促进Al3+释放,但会使F-吸附量减少,这是因为伴随Al3+的释放,部分F-又可以AlF络合物的形态重新进入溶液,尽管在低pH条件下,土壤表面以带正电荷为主而有利于F-吸附. 草酸和抗坏血酸对土壤吸附F-均有抑制作用,但对F-溶出土壤Al3+有促进作用. 此外,草酸对土壤铁氧化物的选择性溶解作用,可使更多F-吸附在土壤铝氧化物位点,并导致Al3+释放量增加.      

有机酸溶解砖红壤过程中Mn（Ⅱ）的释放规律

研究土壤Mn（Ⅱ）释放规律对揭示锰氧化物的形成机制和了解酸性土壤锰毒效应大小具有重要意义.结果表明,柠檬酸溶解砖红壤过程中,Mn（Ⅱ）的释放速率在前4 h比较迅速,其释放数量可达24 h反应时间内总释放量的59.5%,但随后释放速率逐渐减缓.快速阶段被认为是土壤表面交换态Mn（Ⅱ）的释放,而慢速阶段则与土壤锰氧化物的缓...     

海南岛儿童发钙量与土壤交换性钙关系的探讨

通过对海南岛上万名学龄前儿童头发钙含量以及所处地域农耕旱地土壤交换性钙的调查与分析发现：土壤钙与儿童头发钙含量呈极显著正相关;海南岛儿童头发钙均值低于国内其它地方的报道值;土壤环境钙含量的高低,能间接反映人体钙的营养状况。     

呋喃丹对海南花岗岩砖红壤微生物种群的影响

在室温下培养土样并采用梯度稀释涂布的方法研究了不同质量分数的呋喃丹对砖红壤中细菌、真菌和放线菌3大主要土壤微生物种群数量变化的影响。结果表明,细菌、真菌和放线菌种群对呋喃丹的反应随其施加质量分数的不同而有所差别。培养初期,5mg·kg-1呋喃丹处理土壤的细菌、真菌、放线菌数量相对最少。而在整个培养周期内随着培养时间的增加,各处理细菌和放线菌数量均能恢复并接近对照水平,但真菌的生长一直受到抑制且呋喃丹质量分数越大其受抑制程度也越大,表明呋喃丹对细菌和放线菌无明显的影响,而抑制真菌的趋势明显。因此,真菌可以被作为海南砖红壤受呋喃丹污染的敏感指示菌。     

Impacts of simulated acid rain on cation leaching from the Latosol in south China

Acid rain is a problem of increasing agricultural, environmental, and ecological concerns worldwide. This study investigated impacts of simulated acid rain (SAR) on cation leaching from the Latosol in south China. Latosol is an acidic red soil and occurs in the tropical rainforest biome. Laboratory experiments were performed by leaching the soil columns with the SAR at a pH range from 2.5 to 7.0 over a 21-day period. A linear increase in effluent K⁺ concentration was found at the SAR pH 3.0, whereas an exponential decrease in effluent Na⁺ concentration was observed at all levels of the SAR pH. In general, leaching of Ca²⁺ and Mg²⁺ from the Latosol increased as the SAR pH decreased. There was a very good nonlinear correlation between the removal of soil K⁺ and the SAR pH (R² = 0.91), a good nonlinear correlation between the removal of soil Mg⁺² and the SAR pH (R² = 0.83), a fairly good nonlinear correlation between the removal of soil Ca⁺² and the SAR pH (R² = 0.56), and no correlation between the removal of soil Na⁺ and the SAR pH (R² = 0.06). Our study further revealed that the removal of soil cations such as K⁺, Ca⁺², and Mg⁺² can be quantified by the quadratic polynomial equations. In addition, impacts of the SAR on cation leaching depended not only on the SAR pH but also on the original soil pH.