Effect of Co-Use of Fly Ash and Granular Polyacrylamide on Infiltration, Runoff, and Sediment Yield from Sandy Soil under Simulated Rainfall

Coal fly ash (FA) and polyacrylamide (PAM) are two common amendments for improving hydraulic properties of sandy soil. However, their interaction effect on infiltration-runoff processes in sandy soil has been scarcely reported. In this study, FA and anionic PAM granules were mixed thoroughly with a...

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Main Authors: Kai Yang, Zejun Tang, Jianzhang Feng
Format: Article
Language:English
Published: MDPI AG 2020-03-01
Series:Agronomy
Subjects:
Online Access:https://www.mdpi.com/2073-4395/10/3/344
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author Kai Yang
Zejun Tang
Jianzhang Feng
author_facet Kai Yang
Zejun Tang
Jianzhang Feng
author_sort Kai Yang
collection DOAJ
description Coal fly ash (FA) and polyacrylamide (PAM) are two common amendments for improving hydraulic properties of sandy soil. However, their interaction effect on infiltration-runoff processes in sandy soil has been scarcely reported. In this study, FA and anionic PAM granules were mixed thoroughly with a 0&#8722;0.2 m sandy soil layer at FA rates of 0%, 10%, and 15% (<i>w</i>/<i>w</i> soil), and PAM rates of 0%, 0.01%, and 0.02% (<i>w</i>/<i>w</i> soil) along with each FA rate. A simulated rainfall laboratory experiment (slope gradient of 10&#176;, rainfall intensity of 1.5 mm/min) was conducted. During the rainfall, the cumulative runoff yield increased while the average infiltration rate decreased with increasing FA and PAM rates. A higher FA rate of 15% and varying PAM rates resulted in a prominent increase in cumulative sediment yield. After the rainfall, the two-dimensional distribution of water content retained in the soil profile reflected that both FA and PAM increased the water retention capacity of sandy soil, and the effect became more obvious at higher FA and PAM rates. The possible mechanism for the effect of FA and PAM on inhibiting water infiltration during the rainfall and retaining water in the soil layer after the rainfall is attributed to the filling of pores of the coarse soil particles by fine-sized FA particles and flocculation function and binding action of PAM.
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spelling doaj.art-a4e2bf191c7c43a299a6d277879bc9282022-12-21T23:04:11ZengMDPI AGAgronomy2073-43952020-03-0110334410.3390/agronomy10030344agronomy10030344Effect of Co-Use of Fly Ash and Granular Polyacrylamide on Infiltration, Runoff, and Sediment Yield from Sandy Soil under Simulated RainfallKai Yang0Zejun Tang1Jianzhang Feng2Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing 100871, ChinaCollege of Water Resources and Civil Engineering, China Agricultural University, Beijing 100083, ChinaCollege of Water Resources and Civil Engineering, China Agricultural University, Beijing 100083, ChinaCoal fly ash (FA) and polyacrylamide (PAM) are two common amendments for improving hydraulic properties of sandy soil. However, their interaction effect on infiltration-runoff processes in sandy soil has been scarcely reported. In this study, FA and anionic PAM granules were mixed thoroughly with a 0&#8722;0.2 m sandy soil layer at FA rates of 0%, 10%, and 15% (<i>w</i>/<i>w</i> soil), and PAM rates of 0%, 0.01%, and 0.02% (<i>w</i>/<i>w</i> soil) along with each FA rate. A simulated rainfall laboratory experiment (slope gradient of 10&#176;, rainfall intensity of 1.5 mm/min) was conducted. During the rainfall, the cumulative runoff yield increased while the average infiltration rate decreased with increasing FA and PAM rates. A higher FA rate of 15% and varying PAM rates resulted in a prominent increase in cumulative sediment yield. After the rainfall, the two-dimensional distribution of water content retained in the soil profile reflected that both FA and PAM increased the water retention capacity of sandy soil, and the effect became more obvious at higher FA and PAM rates. The possible mechanism for the effect of FA and PAM on inhibiting water infiltration during the rainfall and retaining water in the soil layer after the rainfall is attributed to the filling of pores of the coarse soil particles by fine-sized FA particles and flocculation function and binding action of PAM.https://www.mdpi.com/2073-4395/10/3/344runoffsedimenterosioninfiltrationamendment
spellingShingle Kai Yang
Zejun Tang
Jianzhang Feng
Effect of Co-Use of Fly Ash and Granular Polyacrylamide on Infiltration, Runoff, and Sediment Yield from Sandy Soil under Simulated Rainfall
Agronomy
runoff
sediment
erosion
infiltration
amendment
title Effect of Co-Use of Fly Ash and Granular Polyacrylamide on Infiltration, Runoff, and Sediment Yield from Sandy Soil under Simulated Rainfall
title_full Effect of Co-Use of Fly Ash and Granular Polyacrylamide on Infiltration, Runoff, and Sediment Yield from Sandy Soil under Simulated Rainfall
title_fullStr Effect of Co-Use of Fly Ash and Granular Polyacrylamide on Infiltration, Runoff, and Sediment Yield from Sandy Soil under Simulated Rainfall
title_full_unstemmed Effect of Co-Use of Fly Ash and Granular Polyacrylamide on Infiltration, Runoff, and Sediment Yield from Sandy Soil under Simulated Rainfall
title_short Effect of Co-Use of Fly Ash and Granular Polyacrylamide on Infiltration, Runoff, and Sediment Yield from Sandy Soil under Simulated Rainfall
title_sort effect of co use of fly ash and granular polyacrylamide on infiltration runoff and sediment yield from sandy soil under simulated rainfall
topic runoff
sediment
erosion
infiltration
amendment
url https://www.mdpi.com/2073-4395/10/3/344
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AT jianzhangfeng effectofcouseofflyashandgranularpolyacrylamideoninfiltrationrunoffandsedimentyieldfromsandysoilundersimulatedrainfall