Factors Affecting Tufa Degradation in Jiuzhaigou National Nature Reserve, Sichuan, China

Water and tufa samples were collected from Arrow Bamboo Lake, the stream from Panda Lake to Five-Color Lake, Pearl Shoal and Shuzheng Lakes in Jiuzhaigou National Nature Reserve, China, between October 2013 and September 2014, to investigate tufa growth rate and water environment (water temperature,...

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Main Author: Lixia Liu
Format: Article
Language:English
Published: MDPI AG 2017-09-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/9/9/702
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spelling doaj-428324ed69a5435d9328ce8d8f44ab1f2020-11-24T23:06:48ZengMDPI AGWater2073-44412017-09-019970210.3390/w9090702w9090702Factors Affecting Tufa Degradation in Jiuzhaigou National Nature Reserve, Sichuan, ChinaLixia Liu0Department of Environment, College of Architecture and Environment, Sichuan University, Chengdu 610065, ChinaWater and tufa samples were collected from Arrow Bamboo Lake, the stream from Panda Lake to Five-Color Lake, Pearl Shoal and Shuzheng Lakes in Jiuzhaigou National Nature Reserve, China, between October 2013 and September 2014, to investigate tufa growth rate and water environment (water temperature, pH, electric conductivity, major ions and nutrients), and analyzed to explore the main causes of tufa degradation. The mean annual rate of tufa growth was low and varied within lakes, with the maximum deposit thickness of 332 μm/y. The calcite saturation index ranged from 0.65 to 0.83. Scanning electron microscope images showed that the tufa deposits had non-isopachous structures, and diatoms were the dominant microorganisms that participated in tufa deposition. Porous and crystalline structures of deposits were linked with a high tufa growth and small amounts of diatoms. Conversely, tufa deposits with amorphous and loose structures showed a low crystal growth rate and a high number of diatoms. A one-way analysis of variance and a least significant difference test were applied to identify site differences in water chemistry. Linear correlations indicated that nitrate, phosphate and sulfate inhibit tufa growth (p < 0.05). Increased nitrogen and phosphorus concentrations that originate mainly from atmospheric pollution and tourist activities at scenic attractions could trigger excessive diatom growth, which inhibits tufa precipitation. A series of measures should be implemented (e.g., the visitor number and vehicles should be regulated and controlled) to minimize tufa degradation in the Jiuzhaigou National Nature Reserve.https://www.mdpi.com/2073-4441/9/9/702tufaaquatic environmentdiatomnutrientstatistical analysisone-way ANOVAtourist attraction
collection DOAJ
language English
format Article
sources DOAJ
author Lixia Liu
spellingShingle Lixia Liu
Factors Affecting Tufa Degradation in Jiuzhaigou National Nature Reserve, Sichuan, China
Water
tufa
aquatic environment
diatom
nutrient
statistical analysis
one-way ANOVA
tourist attraction
author_facet Lixia Liu
author_sort Lixia Liu
title Factors Affecting Tufa Degradation in Jiuzhaigou National Nature Reserve, Sichuan, China
title_short Factors Affecting Tufa Degradation in Jiuzhaigou National Nature Reserve, Sichuan, China
title_full Factors Affecting Tufa Degradation in Jiuzhaigou National Nature Reserve, Sichuan, China
title_fullStr Factors Affecting Tufa Degradation in Jiuzhaigou National Nature Reserve, Sichuan, China
title_full_unstemmed Factors Affecting Tufa Degradation in Jiuzhaigou National Nature Reserve, Sichuan, China
title_sort factors affecting tufa degradation in jiuzhaigou national nature reserve, sichuan, china
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2017-09-01
description Water and tufa samples were collected from Arrow Bamboo Lake, the stream from Panda Lake to Five-Color Lake, Pearl Shoal and Shuzheng Lakes in Jiuzhaigou National Nature Reserve, China, between October 2013 and September 2014, to investigate tufa growth rate and water environment (water temperature, pH, electric conductivity, major ions and nutrients), and analyzed to explore the main causes of tufa degradation. The mean annual rate of tufa growth was low and varied within lakes, with the maximum deposit thickness of 332 μm/y. The calcite saturation index ranged from 0.65 to 0.83. Scanning electron microscope images showed that the tufa deposits had non-isopachous structures, and diatoms were the dominant microorganisms that participated in tufa deposition. Porous and crystalline structures of deposits were linked with a high tufa growth and small amounts of diatoms. Conversely, tufa deposits with amorphous and loose structures showed a low crystal growth rate and a high number of diatoms. A one-way analysis of variance and a least significant difference test were applied to identify site differences in water chemistry. Linear correlations indicated that nitrate, phosphate and sulfate inhibit tufa growth (p < 0.05). Increased nitrogen and phosphorus concentrations that originate mainly from atmospheric pollution and tourist activities at scenic attractions could trigger excessive diatom growth, which inhibits tufa precipitation. A series of measures should be implemented (e.g., the visitor number and vehicles should be regulated and controlled) to minimize tufa degradation in the Jiuzhaigou National Nature Reserve.
topic tufa
aquatic environment
diatom
nutrient
statistical analysis
one-way ANOVA
tourist attraction
url https://www.mdpi.com/2073-4441/9/9/702
work_keys_str_mv AT lixialiu factorsaffectingtufadegradationinjiuzhaigounationalnaturereservesichuanchina
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