A Portable Device for On‐Site Measurement of Sediment Concentration Through Volume‐Mass Replacement

Author:

Yue Qiuxing1ORCID,Zhan Xiaoyun12ORCID,Guo Minghang12,Zhao Jun12,Liu Baoyuan12

Affiliation:

1. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau Northwest A&F University Yangling Shanxi China

2. Institute of Soil and Water Conservation Chinese Academy of Sciences and Ministry of Water Resources Yangling Shanxi China

Abstract

AbstractTo enable on‐site and near‐real‐time sediment concentration measurements, a novel type of portable device with a constant volume sampling bottle was developed in this study. The device consisted of a sampling bottle, a measuring assembly, and a platform for auxiliary data management. Five representative soils and eight sediment concentrations were used to validate the device accuracy and application. Moreover, a novel concept of sediment effective density (SED) was proposed. Under SED, a linear regression was fit between the measured and actual sediment concentrations. The results revealed that the slopes of the fitting line were close to 1, and the R2 values were greater than 0.999 for five soils. Moreover, for total samples, the root mean square error (RMSE) and Nash–Sutcliffe efficiency coefficient (NSE) values were 5.59 g/L and 0.9996, respectively. Additionally, an average SED of 2.51 g/cm3 was calculated in this study. With an average soil SED of 2.51 g/cm3 and an average soil solid density of 2.65 g/cm3, the RMSE and NSE were 11.85 and 18.50 g/L and 0.9981 and 0.9954, respectively. This result demonstrated that the designed device accurately measured sediment concentration under various conditions. Furthermore, relative to the traditional oven‐drying method, the device could measure sediment concentration near‐real‐time and with high accuracy, which could be useful for researchers with excellent potential. It was recommended to measure the SED in a laboratory or runoff plot because the sediment sources could be identified and obtained. In a field or river, it was recommended to use 2.51 g/cm3 as the SED, which was more accurate than 2.65 g/cm3.

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

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