Spatial and seasonal distribution of carbon, nitrogen, phosphorus, and sulfur and their ecological stoichiometry in wetland soils along a water and salt gradient in the Yellow River Delta, China

• Published in: Physics and chemistry of the earth. Parts A/B/C Vol. 104; pp. 9 - 17
• Main Authors: Lu, Qiongqiong, Bai, Junhong, Zhang, Guangliang, Zhao, Qingqing, Wu, Jianjun
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.04.2018
• Subjects: C:N:P:S; Carbon; Coastal wetland; Nitrogen; Phosphorous; Sulfur; Phosphorous; Nitrogen; Sulfur; Coastal wetland; Carbon; C:N:P:S
• ISSN: 1474-7065; 1873-5193
• DOI: 10.1016/j.pce.2018.04.001

Top soils (0–10 cm) were collected in three sampling belts during four seasons in 2014, including bare land (HN1), Calamagrostis epigeios (HN2), Typha orientalis (HN3), Phragmites australis (HN4), Tamarix chinensis (HN5) and Suaeda salsa (HN6) along a water and salinity gradient in the Yellow River Delta, China. Soil organic carbon (SOC), total nitrogen (TN), total phosphorous (TP), total sulfur (TS) and their ecological stoichiometry were measured to investigate their seasonal and horizontal distribution patterns, as well as their important influencing factors such as electric conductivity (EC) and water content (WC). Our results showed that the contents of SOC and TN exhibited similar changing tendency along the water and salinity gradient. The TP contents followed the order HN5 ≈ HN2 > HN3 ≈ HN6 > HN4 > HN1. TS levels generally increased with increasing salinity from HN1 to HN6. The higher levels of SOC and TP were mostly observed in October and August, respectively, while the seasonal variations in TN were heterogeneous under different plant covers. TS contents were lower in August compared with other sampling periods except for HN4. The mean values of the C/N, C/P and C/S ratios along a water-salinity gradient ranged from 26 to 72, 20 to 74, and 61 to 292, respectively. Generally, higher C/P ratios were observed in sampling sites with plant covers in October expect for HN1, whereas they were lower in January or August. SOC, TN and TP were significantly positively correlated with soil organic matter (SOM), silt, WC and cation exchange capacity (CEC) (p < 0.05), whereas TS showed a positive correlation with EC and cations content (p > 0.05). Bulk density (BD) had a great influence on C/N ratio, C/P ratio were mainly effected by SOM, EC and silt, while C/S ratio showed a significant negative correlation with BD, EC, K+, Na+, and Mg2+ (p < 0.05). •SOC and TN exhibited similar changing tendency along the salinity gradient.•TS levels generally increased with increasing salinity.•SOC, TP and TS contents showed similar seasonal variation among different sites.•C/N and C/P ratios were mainly effected by SOM, BD, moisture and silt.•C/S ratio showed a negative correlation with EC, K+, Na+, and Mg2+.