题名 | Reply to Comment by Roques et al. on "Base Flow Recession from Unsaturated-Saturated Porous Media considering Lateral Unsaturated Discharge and Aquifer Compressibility" |
作者 | |
通讯作者 | Liang, Xiuyu; Zhan, Hongbin |
发表日期 | 2018-04
|
DOI | |
发表期刊 | |
ISSN | 0043-1397
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EISSN | 1944-7973
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卷号 | 54期号:4页码:3220-3222 |
摘要 | Roques et al. (2018, https://doi. org/10.1002/2017WR022085) claims that they have proposed an exponential time step (ETS) method to improve the computing method of Liang et al. (2017, https://doi. org/ 10.1002/2017WR020938) which used a constant time step (CTS) method on the derivative for dQ/dt in field data, where Q is the base flow discharge and t is the time since the start of base flow recession. This reply emphasizes that the main objective of Liang et al. (2017, https://doi. org/10.1002/2017WR020938) was to develop an analytical model to investigate the effects of the unsaturated flow on base flow recession, not on the data interpretation methods. The analytical model indicates that the base flow recession hydrograph behaves as dQ/dt similar to aQ(b) with the exponent b close to 1 at late times, which is consistent with previous theoretical models. The model of Liang et al. (2017, https://doi. org/10.1002/2017WR020938) was applied to field data where the derivative of dQ/dt was computed using the CTS method, a method that has been widely adopted in previous studies. The ETS method proposed by Roques et al. (2017, https://doi. org/10.1016/j. advwatres. 2017.07.013) appears to be a good alternative but its accuracy needs further validation. Using slopes to fit field data as proposed by Roques et al. (2018, https://doi. org/10.1002/2017WR022085) appears to match data satisfactorily at early times whereas it performs less satisfactorily at late times and leads to the exponent b being obviously larger than 1. |
相关链接 | [来源记录] |
收录类别 | |
语种 | 英语
|
学校署名 | 第一
; 通讯
|
WOS研究方向 | Environmental Sciences & Ecology
; Marine & Freshwater Biology
; Water Resources
|
WOS类目 | Environmental Sciences
; Limnology
; Water Resources
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WOS记录号 | WOS:000434186400041
|
出版者 | |
EI入藏号 | 20181404983310
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EI主题词 | Analytical models
; Aquifers
; HTTP
; Porous materials
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EI分类号 | Groundwater:444.2
; Aerodynamics, General:651.1
; Mathematics:921
; Materials Science:951
|
ESI学科分类 | ENVIRONMENT/ECOLOGY
|
来源库 | Web of Science
|
引用统计 |
被引频次[WOS]:0
|
成果类型 | 期刊论文 |
条目标识符 | http://sustech.caswiz.com/handle/2SGJ60CL/27887 |
专题 | 工学院_环境科学与工程学院 |
作者单位 | 1.Southern Univ Sci & Technol, Sch Environm Sci & Engn, Shenzhen, Guangdong, Peoples R China 2.Texas A&M Univ, Dept Geol & Geophys, College Stn, TX 77843 USA 3.Univ Iowa, Iowa Geol Survey, Iowa City, IA USA |
第一作者单位 | 环境科学与工程学院 |
通讯作者单位 | 环境科学与工程学院 |
第一作者的第一单位 | 环境科学与工程学院 |
推荐引用方式 GB/T 7714 |
Liang, Xiuyu,Zhan, Hongbin,Zhang, You-Kuan,et al. Reply to Comment by Roques et al. on "Base Flow Recession from Unsaturated-Saturated Porous Media considering Lateral Unsaturated Discharge and Aquifer Compressibility"[J]. WATER RESOURCES RESEARCH,2018,54(4):3220-3222.
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APA |
Liang, Xiuyu,Zhan, Hongbin,Zhang, You-Kuan,&Schilling, Keith.(2018).Reply to Comment by Roques et al. on "Base Flow Recession from Unsaturated-Saturated Porous Media considering Lateral Unsaturated Discharge and Aquifer Compressibility".WATER RESOURCES RESEARCH,54(4),3220-3222.
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MLA |
Liang, Xiuyu,et al."Reply to Comment by Roques et al. on "Base Flow Recession from Unsaturated-Saturated Porous Media considering Lateral Unsaturated Discharge and Aquifer Compressibility"".WATER RESOURCES RESEARCH 54.4(2018):3220-3222.
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