Effects of freshwater inputs on soil quality in the Yellow River Delta, China

被引:27
作者
Zhao, Qingqing [1 ]
Bai, Junhong [2 ]
Gao, Yongchao [1 ]
Zhao, Haixiao [1 ]
Huang, Yujie [1 ]
Zhang, Wen [1 ]
Wang, Jianing [1 ]
Chen, Guanhong [1 ]
机构
[1] Qilu Univ Technol, Shandong Acad Sci, Inst Ecol, Shandong Prov Key Lab Appl Microbiol, Jinan 250103, Shandong, Peoples R China
[2] Beijing Normal Univ, Sch Environm, State Key Lab Water Environm Simulat, Beijing 100875, Peoples R China
基金
中国国家自然科学基金;
关键词
Freshwater inputs; Soil quality assessment; Salinity; The minimum data set; Wetland restoration; WETLAND RESTORATION; ORGANIC-MATTER; CROPPING SYSTEMS; SALT-MARSH; INDICATORS; CARBON; DEGRADATION; MANAGEMENT; SUCCESS; RANGELANDS;
D O I
10.1016/j.ecolind.2018.11.041
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
With the degradation or loss of coastal wetlands, more and more restoration projects have been widely conducted. Freshwater inputs have been proved to be an effective restoration way for degraded coastal wetlands. However, little information is available on the changes in soil quality caused by freshwater inputs. Soil samples were collected to a depth of 50 cm in freshwater restoration wetlands (FRW), tidal salt marshes with Suaeda salsa (SSM) and tidal salt marshes with Tamarix chinensis (TSM) in the Yellow River Delta, China, in August 2015, to investigate the changes in soil quality after freshwater inputs. Our results showed that soil salinity was significantly higher in natural wetlands than that in freshwater restoration wetlands (p < 0.05), while no significant differences in soil organic matter (SOM) were observed among three wetlands (p > 0.05). Cluster analysis and principal component analysis exhibited that soil samples in natural wetlands and freshwater restoration wetlands were clearly distinguished. Soil properties were screened and transformed to establish a soil quality index (SQI) for the assessment of soil quality. Soil salinity, SOM and silt were selected in the minimum data set in this study. Although there were no statistical differences in SQIs (p > 0.05), both linear SQI (SQI(L)) and non-linear SQI (SQI(NL)) for three wetlands followed the order: SSM > FRW > TSM. And the SQI(L) values were lower compared with SQI(NL). The contributions of soil salinity to SQI(L) for three wetlands and SQI(NL) for TSM and SSM were the highest in the minimum data for three wetlands, while SOM showed the highest contribution proportion of SQI(NL) for FRW.
引用
收藏
页码:619 / 626
页数:8
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