the study on the composition of interstitial water in the sediment shows that diagenesis environment is mainly a reductive environment.
通过对巖心沉积物间隙水成分的研究,表明成巖环境主要为还原环境。
concentrations of do, tn, tp, din, po_(4)-p, and fe in bottom water, din, po_(4)-p and fe in interstitial water and grain size and organic carbon in surface sediments of the jiaozhou bay are analyzed.
the nitrogen distribution and release to the overlying water and interstitial water through a series of large static simulating experiments were probed into.
通过大型静态土柱模拟实验,研究氮在上覆水和孔隙水中的分布特性和释放特性。
it is obvious that the the distribution of silica acid in interstitial water were affected by the contents of biogenic silica and aluminium, and aquiferous proportion as well.
通过分析发现影响同航次间隙水中硅酸分布的因素主要是生物硅含量、铝含量和含水率。
with the exception of nh_4-n, the interstitial water shows no_3-n concentration 17.8 times, no_(2)-n 9.3 times, po_(4)-p 12.5 times, and fe 7.7 times higher than the counterparts of the bottom water.