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Aug 30, 2021

Erratum for “Experimental Study on the Performance of a Sand Filtration Method and Device by Using Natural Soils and Subsurface PVC Drainage Pipes” by Tian Xia, Juncang Tian, and Wenping Fei

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Publication: Journal of Irrigation and Drainage Engineering
Volume 147, Issue 11
During composition, a conversion error resulted in several incorrect values. The following changes should be made:
1.
In the “Experimental Material and Preparation” section:
1  m3” should be “104  m3.”
Two instances of “135  g/m3” should be “1.35×106  g/m3.”
Two instances of “143  g/m3” should be “1.43×106  g/m3.”
131  g/m3” should be “1.31×106  g/m3.”
2.
In the “Experimental Method” section:
1  m3” should be “104  m3.”
250280  g/m3” should be “2.52.8×106  g/m3.”
265  g/m3” should be “2.65×106  g/m3.”
3.
In the “Filtration Velocity of the Filtered Water” section, in order to match the corresponding units of measure presented in Figs. 4 and 5:
0.0178  m/h” should be “1.78  cm/h.”
0.0075  m/h” should be “0.75  cm/h.”
4.
In the “Impact of Sandy Water Filtration on Soil Physical Properties” section:
112  g/m3” should be “1.12×106  g/m3.”
128  g/m3” should be “1.28×106  g/m3.”
020.4  m” should be “0.20.4  m.”
163  g/m3” should be “1.63×106  g/m3.”
135  g/m3” should be “1.35×106  g/m3.”
151  g/m3” should be “1.51×106  g/m3.”
143  g/m3” should be “1.43×106  g/m3.”
5.
Tables 1 and 2 included conversion errors in the “Bulk density (g/m3)” columns and the footnotes. Table 1 also contained a typographical error in the “Depth (m)” column. The correct tables are provided herein.
Table 1. Physical properties of disturbed soil (sandy loam soil as filter media)
Depth (m)Particle size distributionBulk density (g/m3)PorosityPore size distribution
Clay (%)Silt (%)Sand (%)30 μm–1 mm (%)200 nm–30 μm (%)
0–0.212.6351.0436.331.44×1060.455.324.6
0.2–0.413.1451.3335.531.72×1060.356.422.5
0.4–0.613.8355.4430.731.68×1060.365.720.9
0.6–0.813.5054.9531.551.75×1060.336.019.8
0.8–113.4351.5934.981.57×1060.405.821.7

Note: Physical properties of undisturbed sandy loam soil = clay 5.45%, silt 32.05%, and sand 62.50%; bulk density 1.35×106  g/m3; porosity 0.49; transmission pores (effective diameter 30 μm–1 mm) occupying 14.1% of the total pore space; and storage pores (effective diameter 200 nm–30 μm) occupying 19.2% of the total pore space. The amount of macro pores (effective diameter 1–10 mm) is tiny and is not taken into consideration.

Table 2. Physical properties of disturbed soil (sandy soil as filter media)
Depth (m)Particle size distributionBulk density (g/m3)PorosityPore size distribution
Clay (%)Silt (%)Sand (%)30 μm–1 mm (%)200 nm–30 μm (%)
0–0.218.8610.1870.961.47×1060.4213.819.4
0.2–0.419.5610.3270.121.49×1060.4412.918.9
0.4–0.620.1810.5169.311.53×1060.4112.218.3
0.6–0.820.5310.7768.701.54×1060.4211.919.1
0.8–120.7211.1268.261.53×1060.3911.418.5

Note: Physical properties of undisturbed sandy soil = clay 7.73%, silt 6.31%, and sand 85.96%; bulk density 1.43×106  g/m3; porosity 0.46; transmission pores (effective diameter 30 μm–1 mm) occupying 26.5% of the total pore space; and storage pores (effective diameter 200 nm–30 μm) occupying 9.4% of the total pore space. The amount of macro pores (effective diameter 1–10 mm) is tiny and is not taken into consideration.

ASCE regrets the errors.

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Go to Journal of Irrigation and Drainage Engineering
Journal of Irrigation and Drainage Engineering
Volume 147Issue 11November 2021

History

Received: Apr 26, 2021
Accepted: Jul 30, 2021
Published online: Aug 30, 2021
Published in print: Nov 1, 2021
Discussion open until: Jan 30, 2022

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Ph.D. Student, School of Civil and Hydraulic Engineering, Ningxia Univ., Yinchuan 750021, China. Email: [email protected]
Juncang Tian [email protected]
Professor, School of Civil and Hydraulic Engineering, Ningxia Univ., Yinchuan 750021, China; Director, Ningxia Research Center of Technology on Water-saving Irrigation and Water Resources Regulation, Ningxia Univ., Yinchuan 750021, China; Director, Center of Engineering Research on Efficient Utilization of Water Resources in Modern Agriculture in Arid Regions, Ministry of Education, Ningxia Univ., Yinchuan 750021, China (corresponding author). Email: [email protected]; [email protected]
Wenping Fei [email protected]
Associate Professor, State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resources and Hydropower, Sichuan Univ., Chengdu 610065, China. Email: [email protected]

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