Variation Characteristics of the Main Hydrochemical Indexes in Typical Subterranean Rivers in the South China Karst Region Based on Curve Fitting

The water quality of subterranean rivers in the South China Karst region has undergone dramatic changes resulting from industrial and social development over the past 60 years. The combination of sampling results from subterranean rivers in four typical study areas in the South China Karst region fr...

Full description

Bibliographic Details
Main Authors: Shuyi Liu, Chuan Liang, Lina Wang, Lingwei Zeng, Chunyi Wang
Format: Article
Language:English
Published: Hindawi Limited 2019-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1155/2019/2787349
id doaj-563304fc8dca4455a9334a5511f96c9f
record_format Article
spelling doaj-563304fc8dca4455a9334a5511f96c9f2020-11-25T00:07:01ZengHindawi LimitedThe Scientific World Journal2356-61401537-744X2019-01-01201910.1155/2019/27873492787349Variation Characteristics of the Main Hydrochemical Indexes in Typical Subterranean Rivers in the South China Karst Region Based on Curve FittingShuyi Liu0Chuan Liang1Lina Wang2Lingwei Zeng3Chunyi Wang4College of Water Resource and Hydropower, Sichuan University, Chengdu, ChinaCollege of Water Resource and Hydropower, Sichuan University, Chengdu, ChinaCollege of Cyber Security, Sichuan University, Chengdu, ChinaThe Engineering Department, Shanghai Foundation Engineering Group Co., Ltd, Shenzhen, ChinaCollege of Water Resource and Hydropower, Sichuan University, Chengdu, ChinaThe water quality of subterranean rivers in the South China Karst region has undergone dramatic changes resulting from industrial and social development over the past 60 years. The combination of sampling results from subterranean rivers in four typical study areas in the South China Karst region from October to December 2015 (dry season) and correlation analysis using SPSS revealed that the main ions K+, Na+, and SO42- exhibited a significant correlation (p<0.01) and that Ca2+, HCO3-, and Mg2+ exhibited a good correlation (p<0.01). Additionally, we consolidated the data collected since 1960 and, by applying MATLAB, a variety of fitting curve methods were used to fit all the data, and the results showed that cubic spline interpolation fitting performed the best. The squared correlation coefficients (R2) of the obtained fitting curves for Ca2+, HCO3-, and Mg2+ are 0.8545, 0.8689, and 0.7632, respectively, and the corrected R2 values are 0.6739, 0.7088, and 0.4853, respectively. The R2 values of the obtained fitting curves for K+, Na+, Cl-, SO42-, and NO3- are 0.9085, 0.8964, 0.7531, 0.6222, and 0.7997, respectively, and the corrected R2 values are 0.7904, 0.7669, 0.5272, 0.2815, and 0.6127, respectively, indicating excellent fits. Based on the fitting curves, the overall water quality conditions in the karst region were analyzed and compared. Finally, the development of subterranean rivers in the South China Karst region was determined. Based on the results, the following conclusions can be drawn: the development of the subterranean rivers is indeed a slow process, but water quality can change rapidly in response to the transformation of industrial society. Additionally, the results indicate the crucial importance of urban planning that takes into account environmental protection during development in karst regions. This study aims to provide a basis for the management of karst areas and the improvement of groundwater quality by evaluating geochemical processes.http://dx.doi.org/10.1155/2019/2787349
collection DOAJ
language English
format Article
sources DOAJ
author Shuyi Liu
Chuan Liang
Lina Wang
Lingwei Zeng
Chunyi Wang
spellingShingle Shuyi Liu
Chuan Liang
Lina Wang
Lingwei Zeng
Chunyi Wang
Variation Characteristics of the Main Hydrochemical Indexes in Typical Subterranean Rivers in the South China Karst Region Based on Curve Fitting
The Scientific World Journal
author_facet Shuyi Liu
Chuan Liang
Lina Wang
Lingwei Zeng
Chunyi Wang
author_sort Shuyi Liu
title Variation Characteristics of the Main Hydrochemical Indexes in Typical Subterranean Rivers in the South China Karst Region Based on Curve Fitting
title_short Variation Characteristics of the Main Hydrochemical Indexes in Typical Subterranean Rivers in the South China Karst Region Based on Curve Fitting
title_full Variation Characteristics of the Main Hydrochemical Indexes in Typical Subterranean Rivers in the South China Karst Region Based on Curve Fitting
title_fullStr Variation Characteristics of the Main Hydrochemical Indexes in Typical Subterranean Rivers in the South China Karst Region Based on Curve Fitting
title_full_unstemmed Variation Characteristics of the Main Hydrochemical Indexes in Typical Subterranean Rivers in the South China Karst Region Based on Curve Fitting
title_sort variation characteristics of the main hydrochemical indexes in typical subterranean rivers in the south china karst region based on curve fitting
publisher Hindawi Limited
series The Scientific World Journal
issn 2356-6140
1537-744X
publishDate 2019-01-01
description The water quality of subterranean rivers in the South China Karst region has undergone dramatic changes resulting from industrial and social development over the past 60 years. The combination of sampling results from subterranean rivers in four typical study areas in the South China Karst region from October to December 2015 (dry season) and correlation analysis using SPSS revealed that the main ions K+, Na+, and SO42- exhibited a significant correlation (p<0.01) and that Ca2+, HCO3-, and Mg2+ exhibited a good correlation (p<0.01). Additionally, we consolidated the data collected since 1960 and, by applying MATLAB, a variety of fitting curve methods were used to fit all the data, and the results showed that cubic spline interpolation fitting performed the best. The squared correlation coefficients (R2) of the obtained fitting curves for Ca2+, HCO3-, and Mg2+ are 0.8545, 0.8689, and 0.7632, respectively, and the corrected R2 values are 0.6739, 0.7088, and 0.4853, respectively. The R2 values of the obtained fitting curves for K+, Na+, Cl-, SO42-, and NO3- are 0.9085, 0.8964, 0.7531, 0.6222, and 0.7997, respectively, and the corrected R2 values are 0.7904, 0.7669, 0.5272, 0.2815, and 0.6127, respectively, indicating excellent fits. Based on the fitting curves, the overall water quality conditions in the karst region were analyzed and compared. Finally, the development of subterranean rivers in the South China Karst region was determined. Based on the results, the following conclusions can be drawn: the development of the subterranean rivers is indeed a slow process, but water quality can change rapidly in response to the transformation of industrial society. Additionally, the results indicate the crucial importance of urban planning that takes into account environmental protection during development in karst regions. This study aims to provide a basis for the management of karst areas and the improvement of groundwater quality by evaluating geochemical processes.
url http://dx.doi.org/10.1155/2019/2787349
work_keys_str_mv AT shuyiliu variationcharacteristicsofthemainhydrochemicalindexesintypicalsubterraneanriversinthesouthchinakarstregionbasedoncurvefitting
AT chuanliang variationcharacteristicsofthemainhydrochemicalindexesintypicalsubterraneanriversinthesouthchinakarstregionbasedoncurvefitting
AT linawang variationcharacteristicsofthemainhydrochemicalindexesintypicalsubterraneanriversinthesouthchinakarstregionbasedoncurvefitting
AT lingweizeng variationcharacteristicsofthemainhydrochemicalindexesintypicalsubterraneanriversinthesouthchinakarstregionbasedoncurvefitting
AT chunyiwang variationcharacteristicsofthemainhydrochemicalindexesintypicalsubterraneanriversinthesouthchinakarstregionbasedoncurvefitting
_version_ 1725420360279523328