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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
EISSN
1944-7973
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
SCI ; EI
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
WOS记录号
WOS:000434186400041
出版者
EI入藏号
20181404983310
EI主题词
Analytical models ; Aquifers ; HTTP ; Porous materials
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.
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.
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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