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Spatial and seasonal distributions of soil sulfur in two marsh wetlands with different flooding frequencies of the Yellow River Delta, China

机译:spatial and seasonal distributions of soil sulfur in two marsh wetlands with different flooding frequencies of the Yellow River Delta, China

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摘要

Soil samples from 0 to 100 cm depth were collected in eight sampling sites (Sites A1, B1, C1 and D1; Sites A2, B2, C2 and D2) respectively along two 250-m length of sampling zones (Zone N and Zone S) from the Yellow River channel to a tidal creek in the short-term flooding and seasonal flooding wetland of the Yellow River Delta of China in fall of 2007 and spring of 2008 to investigate spatial and seasonal distribution patterns of total sulfur (TS) and their influencing factors. Our results showed that TS contents in both seasons in surface soil in Zone N increased with increasing distances away from the Yellow River channel except for Site D1 in fall. However, TS contents in both seasons in surface soil in Zone S showed a tendency of increasing and then decreasing with increasing distances away from the Yellow River channel. Relative to spring, the mean TS contents in surface soils were slightly higher in fall in Zone N, whereas an opposite tendency was observed in Zone S. The mean TS stocks were obviously higher in fall with 934.36 g/m(2) and 877.77 g/m(2) compared to those in spring with 729.85 g/m(2) and 696.78 g/m(2) in Zone Nand Zone S, respectively. TS contents and stock generally declined with depth along soil profiles with one accumulation peaks at a soil increment of 40-60 cm. Topsoil concentration factors also indicated that TS had shallower distribution in soil profiles. Soil total carbon (TC), total nitrogen (TN), soil organic matter( SOM), salinity and silt exerted positive loadings on TS, while soil pH and depth exhibited a negative correlation with TS content. (C) 2015 Elsevier B.V. All rights reserved.
机译:沿着两个长度为250 m的采样区(N区和S区)分别在八个采样点(站点A1,B1,C1和D1;站点A2,B2,C2和D2)收集了0至100 cm深度的土壤样本。 2007年秋季和2008年春季,在黄河三角洲的短期洪水和季节性洪水湿地中,从黄河航道到潮汐小溪,研究了总硫(TS)的时空分布格局及其影响因素。我们的结果表明,除秋季的站点D1外,N区表层土壤中两个季节的TS含量均随着距黄河河道的距离的增加而增加。但是,随着距黄河河道的距离增加,S区表层土壤中两个季节的TS含量均呈先升高后降低的趋势。相对于春季,N区的秋季土壤表层土壤平均TS含量略高,而S区则呈现相反的趋势。秋季,TS土壤的平均TS含量明显较高,分别为934.36 g / m(2)和877.77 g / m(2),而春季在区域N和区域S分别为729.85 g / m(2)和696.78 g / m(2)。沿土壤剖面,TS含量和储量通常随深度下降,在40-60 cm的土壤增量处有一个积累峰。表土浓度因子也表明TS在土壤剖面中分布较浅。土壤总碳(TC),总氮(TN),土壤有机质(SOM),盐分和淤泥对TS产生正负荷,而土壤pH和深度与TS含量呈负相关。 (C)2015 Elsevier B.V.保留所有权利。

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