Abstract

In flooded soils, soil–water interface (SWI) is the key zone controlling biogeochemical dynamics. Chemical species and concentrations vary greatly at micro- to cm-scales. Techniques able to track these changing element profiles both in space and over time with appropriate resolution are rare. Here, we report a patent-pending technique, the Integrated Porewater Injection (IPI) sampler, which is designed for soil porewater sampling with minimum disturbance to saturated soil environment. IPI sampler employs a single hollow fiber membrane tube to passively sample porewater surrounding the tube. When working, it can be integrated into the sample introduction system, thus the sample preparation procedure is dramatically simplified. In this study, IPI samplers were coupled to ICP-MS at data-only mode. The limits of detection of IPI-ICP-MS for Ni, As, Cd, Sb, and Pb were 0.12, 0.67, 0.027, 0.029, and 0.074 μg·L–1, respectively. Furthermore, 25 IPI samplers were assembled into an SWI profiler using 3D printing in a one-dimensional array. The SWI profiler is able to analyze element profiles at high spatial resolution (∼2 mm) every ≥24 h. When deployed in arsenic-contaminated paddy soils, it depicted the distributions and dynamics of multiple elements at anoxic–oxic transition. The results show that the SWI profiler is a powerful and robust technique in monitoring dynamics of element profile in soil porewater at high spatial resolution. The method will greatly facilitate studies of elements behaviors in sediments of wetland, rivers, lakes, and oceans.

Highlights

  • Aquatic sediments play an important role as sinks for metals and metalloids.[1]

  • The chemical speciation and mobility of elements are mainly controlled by the redox condition, pH, and organic matter content of the sediments.[2−4] Under natural conditions, a redox transition occurs along the soil−water interface (SWI), and the biogeochemical characters vary at the mm scale in sediment.[5]

  • We investigated the limit of detection (LOD), influences of carrier solution and humc acid (HA), and the characteristics of time-dependent diffusion across the sampling tube

Read more

Summary

Introduction

Aquatic sediments play an important role as sinks for metals and metalloids.[1]. The chemical speciation and mobility of elements are mainly controlled by the redox condition, pH, and organic matter content of the sediments.[2−4] Under natural conditions, a redox transition occurs along the soil−water interface (SWI), and the biogeochemical characters vary at the mm scale in sediment.[5].

Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call