A Hypogene Karst Development Pattern Controlled by the Deep-Cycle of Groundwater in the Syncline in Huanjiang, Guangxi, China
Abstract
:1. Introduction
2. Geologic Setting
3. Methods and Test
3.1. Deep Karstification of Well and Groundwater Sampling
3.2. Regional Hydrogeological Survey and Groundwater Sampling
3.3. Test Methods forf Hydrochemistry
3.4. Test Methods for Stable Isotopes
3.5. Geophysical Interpretation Methods
4. Results
4.1. Hydrogeological Characteristics of Sampling Points
4.2. Geochemistry of Deep Karst Groundwater
4.3. δ2H and δ18O Characteristics of Deep Groundwater
5. Discussion
5.1. Comparative Analysis of Physical Characteristics of Sampling Points
5.2. Hydrochemistry Evolution of Deep Karst Water
5.3. Isotopic Characteristics and Indications of Karst Groundwater
5.4. Hypogene Groundwater Circulation and Hypogene Karst Development Pattern
5.4.1. Bottom of Deep Karst Groundwater Circulation
5.4.2. Hydrodynamic Analysis of Hypogene Karst
5.4.3. Runoff Channels of Hypogene Karst Groundwater
6. Conclusions
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Acknowledgments
Conflicts of Interest
References
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ID | Elevation(m) | Type | Exposed Condition | Temperature (°C)/January | Average Flow in Dry Season (L/s) | Average Flow in Rainy Season (L/s) | Water Table (m) |
---|---|---|---|---|---|---|---|
HD1-2 | 200 | well | C2d/Near the fault | 20~33/depth: 0–850 m | / | / | 7~20 |
HD1-4 | 200 | well | C2d/Near the fault | 20~42/depth: 0–1100 m | / | / | 7~20 |
HS001 | 193 | descending spring | C2h | 21.2 | 5.5 | 30.5 | 0 |
HS002 | 187 | descending spring | C2h | 20.3 | 31 | 70 | 0 |
HS003 | 172 | descending spring | C2h | 21.2 | 20.5 | 69 | 0 |
HS004 | 176 | descending spring | C2h | 19.2 | 62.1 | 115 | 0 |
HS005 | 183 | descending spring | C1d | 19.8 | 2 | 15 | 0 |
HS006 | 252 | ponor | C2d | 16.1 | 10.5 | 80.7 | 1.2 |
HS007 | 334 | puddle | C2d | 19.8 | / | / | 1 |
HS008 | 135 | descending spring | C2d | 20.2 | 93.1 | 174.8 | 0 |
HS009 | 100 | skylight | P1m | 21.2 | / | / | 30 |
HS010 | 113 | ascending spring | Fault | 24.1 | 310.5 | 360.9 | 0 |
HS011 | 92 | skylight | C2m | 20.8 | / | / | 19 |
HS012 | 194 | skylight | C2h | 21.2 | / | / | 21 |
HS013 | 365 | skylight | C1d | 21.6 | / | / | 1.5 |
HS014 | 399 | descending spring | C2d/C1d/On the stratigraphic boundary | 19.6 | 18 | 47 | 0 |
HS015 | 382 | puddle | C1d | 21.3 | / | / | 1.5 |
HS016 | 417 | descending spring | C2h | 20.6 | 0.1 | 1.9 | 0 |
HS017 | 191 | skylight | C2h | 21.2 | 173.1 | 246.7 | 0.9 |
HS018 | 100 | descending spring | C1d | 20.2 | 0.01 | 1.8 | 0 |
HS019 | 122 | pumping well | D3 | 22 | / | / | 18 |
HS020 | 190 | ascending spring | C2d/C1d/On the stratigraphic boundary | 21.8 | 1.8 | 13.9 | 0 |
HS021 | 217 | descending spring | C2h | 20.8 | 20.3 | 48.2 | 0 |
HS022 | 183 | ponor | C2h | 17.3 | 1.1 | 10.5 | 1.3 |
Long River | 110 | river | / | 17.2 | / | / | 0 |
Parameters | Sampling ID | pH | TDS | K+ | Na+ | Ca2+ | Mg2+ | Cl− | SO42− | HCO3− | NO3− |
---|---|---|---|---|---|---|---|---|---|---|---|
ppm | |||||||||||
MIN | HD1-2-shallow | 7.12 | 522.45 | 0.03 | 0.10 | 0.52 | 32.09 | 0.41 | 1.96 | 11.99 | 0.00 |
HD1-2-depth3 | 7.52 | 508.23 | 0.01 | 0.04 | 1.18 | 30.44 | 0.34 | 2.12 | 11.52 | 0.00 | |
HD1-4-shallow | 7.38 | 418.94 | 0.04 | 0.23 | 4.10 | 23.92 | 1.99 | 1.54 | 8.72 | 0.00 | |
HD1-4-depth1 | 7.45 | 459.55 | 0.01 | 0.14 | 6.37 | 25.01 | 2.52 | 3.70 | 7.28 | 0.00 | |
HD1-4-depth2 | 7.43 | 448.41 | 0.04 | 0.14 | 7.44 | 24.28 | 2.63 | 4.69 | 8.02 | 0.00 | |
HS010 | 7.44 | 346.15 | 0.15 | 0.24 | 0.72 | 0.72 | 0.00 | 3.14 | 11.13 | 0.00 | |
Other springs | 7.12 | 485.58 | 0.15 | 0.05 | 62.65 | 5.20 | 1.38 | 5.92 | 227.23 | 0.04 | |
MAX | HD1-2-shallow | 7.82 | 750.88 | 1.04 | 1.19 | 78.84 | 73.19 | 4.17 | 12.17 | 413.51 | 6.94 |
HD1-2-depth3 | 7.99 | 732.08 | 1.05 | 1.11 | 77.29 | 69.56 | 4.12 | 11.78 | 402.91 | 6.12 | |
HD1-4-shallow | 7.81 | 650.88 | 1.22 | 9.01 | 67.25 | 54.86 | 8.53 | 10.69 | 355.18 | 16.12 | |
HD1-4-depth1 | 7.84 | 667.46 | 0.96 | 10.38 | 68.00 | 57.35 | 9.16 | 10.88 | 363.42 | 15.49 | |
HD1-4-depth2 | 8.02 | 868.21 | 2.96 | 66.72 | 63.58 | 54.84 | 49.08 | 97.36 | 371.09 | 18.47 | |
HS010 | 7.88 | 459.38 | 1.47 | 1.64 | 81.87 | 77.93 | 4.92 | 13.92 | 236.02 | 10.71 | |
Other springs | 7.65 | 644.74 | 2.39 | 19.63 | 88.28 | 29.50 | 16.91 | 97.83 | 336.41 | 18.46 | |
MEAN | HD1-2-shallow | 7.57 | 672.33 | 0.28 | 0.53 | 65.78 | 38.22 | 2.24 | 9.09 | 339.60 | 3.86 |
HD1-2-depth3 | 7.68 | 671.16 | 0.21 | 0.54 | 65.99 | 37.71 | 2.08 | 9.21 | 339.82 | 3.80 | |
HD1-4-shallow | 7.59 | 561.53 | 0.50 | 2.82 | 50.41 | 33.60 | 4.13 | 7.83 | 282.21 | 6.14 | |
HD1-4-depth1 | 7.65 | 584.47 | 0.20 | 3.31 | 53.92 | 33.90 | 4.49 | 7.97 | 294.41 | 4.59 | |
HD1-4-depth2 | 7.66 | 632.73 | 0.79 | 14.51 | 52.37 | 32.39 | 11.85 | 22.33 | 303.11 | 5.63 | |
HS010 | 7.58 | 437.76 | 0.46 | 0.65 | 70.71 | 9.32 | 3.09 | 10.40 | 209.56 | 8.05 | |
Other springs | 7.38 | 552.39 | 0.86 | 1.55 | 75.53 | 17.47 | 4.74 | 15.69 | 288.46 | 3.63 | |
STD | HD1-2-shallow | 0.19 | 62.29 | 0.34 | 0.30 | 23.14 | 12.43 | 1.00 | 2.75 | 116.88 | 1.81 |
HD1-2-depth3 | 0.15 | 62.39 | 0.34 | 0.34 | 22.93 | 11.35 | 0.96 | 2.68 | 116.36 | 1.64 | |
HD1-4-shallow | 0.15 | 80.39 | 0.40 | 2.72 | 20.28 | 7.61 | 1.83 | 2.92 | 98.24 | 4.92 | |
HD1-4-depth1 | 0.11 | 68.53 | 0.28 | 3.27 | 18.20 | 8.14 | 1.90 | 2.57 | 100.88 | 4.35 | |
HD1-4-depth2 | 0.17 | 108.20 | 0.88 | 18.52 | 15.81 | 7.98 | 12.91 | 25.40 | 103.17 | 5.72 | |
HS010 | 0.11 | 30.43 | 0.33 | 0.38 | 22.17 | 21.62 | 1.15 | 2.56 | 62.72 | 2.62 | |
Other springs | 0.15 | 42.89 | 0.70 | 4.30 | 7.96 | 7.31 | 4.12 | 19.93 | 29.87 | 5.03 | |
C.V | HD1-2-shallow | 0.02 | 0.09 | 1.23 | 0.57 | 0.35 | 0.33 | 0.45 | 0.30 | 0.34 | 0.47 |
HD1-2-depth3 | 0.02 | 0.09 | 1.63 | 0.62 | 0.35 | 0.30 | 0.46 | 0.29 | 0.34 | 0.43 | |
HD1-4-shallow | 0.02 | 0.14 | 0.80 | 0.96 | 0.40 | 0.23 | 0.44 | 0.37 | 0.35 | 0.80 | |
HD1-4-depth1 | 0.01 | 0.12 | 1.38 | 0.99 | 0.34 | 0.24 | 0.42 | 0.32 | 0.34 | 0.95 | |
HD1-4-depth2 | 0.02 | 0.17 | 1.11 | 1.28 | 0.30 | 0.25 | 1.09 | 1.14 | 0.34 | 1.02 | |
HS010 | 0.01 | 0.07 | 1.38 | 1.71 | 3.19 | 0.43 | 2.68 | 4.07 | 3.34 | 3.08 | |
Other springs | 0.02 | 10.76 | 0.61 | 1.61 | 2.88 | 3.32 | 2.15 | 3.44 | 2.92 | 2.31 |
Index | Parameters | HS010 (‰) | HD1-2 -shallow (‰) | HD1-2 -depth3 (‰) | HD1-4 -shallow (‰) | HD1-4 -depth1 (‰) | HD1-4 -depth2 (‰) | Other Springs (‰) |
---|---|---|---|---|---|---|---|---|
δ2H | min | −48.20 | −53.80 | −52.70 | −48.40 | −48.10 | −47.80 | −59.10 |
max | −44.50 | −44.70 | −45.70 | −46.20 | −44.40 | −45.40 | −35.40 | |
mean | −46.21 | −48.81 | −48.77 | −47.21 | −46.72 | −46.70 | −46.28 | |
STD | 1.28 | 3.20 | 2.50 | 0.69 | 1.25 | 0.84 | 5.29 | |
C.V | 0.03 | 0.07 | 0.05 | 0.01 | 0.03 | −0.02 | 0.11 | |
δ18O | min | −7.34 | −8.05 | −7.96 | −7.44 | −7.37 | −7.35 | −8.80 |
max | −6.95 | −6.95 | −7.09 | −7.07 | −7.20 | −7.03 | −6.36 | |
mean | −7.21 | −7.45 | −7.44 | −7.26 | −7.30 | −7.24 | −7.35 | |
STD | 0.13 | 0.37 | 0.29 | 0.12 | 0.07 | 0.11 | 0.70 | |
C.V | 0.02 | 0.05 | 0.04 | 0.02 | 0.009 | –0.01 | 0.09 |
Ionic Name | K+ | Na+ | Ca2+ | Mg2+ | Cl− | SO42− | HCO3− | CO32− | NO3− | TDS |
---|---|---|---|---|---|---|---|---|---|---|
K+ | 1 | 0.58 | 0.16 | -0.25 | 0.66 | 0.66 | 0.09 | −0.22 | 0.11 | 0.12 |
Na+ | 0.58 | 1 | −0.13 | 0.00 | 0.95 | 0.78 | 0.12 | −0.10 | 0.06 | 0.34 |
Ca2+ | 0.16 | −0.13 | 1 | −0.75 | −0.02 | 0.20 | 0.68 | −0.82 | 0.29 | 0.29 |
Mg2+ | −0.25 | 0.00 | −0.75 | 1 | −0.12 | −0.21 | −0.21 | 0.66 | −0.42 | 0.28 |
Cl− | 0.66 | 0.95 | −0.02 | −0.12 | 1 | 0.82 | 0.11 | −0.15 | 0.20 | 0.28 |
SO42− | 0.66 | 0.78 | 0.20 | −0.21 | 0.82 | 1 | 0.11 | −0.18 | 0.30 | 0.29 |
HCO− | 0.09 | 0.12 | 0.68 | −0.21 | 0.11 | 0.11 | 1 | −0.82 | 0.03 | 0.78 |
CO32− | −0.22 | −0.10 | −0.82 | 0.66 | −0.15 | −0.18 | −0.82 | 1 | −0.32 | 0.33 |
NO− | 0.11 | 0.06 | 0.29 | −0.42 | 0.20 | 0.30 | 0.03 | −0.32 | 1 | 0.17 |
TDS | 0.12 | 0.34 | 0.29 | 0.28 | 0.28 | 0.29 | 0.78 | 0.33 | 0.17 | 1 |
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Dong, H.; Dan, Y.; Liang, J.; Liang, B.; Nie, G.; Ji, S. A Hypogene Karst Development Pattern Controlled by the Deep-Cycle of Groundwater in the Syncline in Huanjiang, Guangxi, China. Water 2021, 13, 199. https://doi.org/10.3390/w13020199
Dong H, Dan Y, Liang J, Liang B, Nie G, Ji S. A Hypogene Karst Development Pattern Controlled by the Deep-Cycle of Groundwater in the Syncline in Huanjiang, Guangxi, China. Water. 2021; 13(2):199. https://doi.org/10.3390/w13020199
Chicago/Turabian StyleDong, Hongqi, Yong Dan, Jiapeng Liang, Bin Liang, Guoquan Nie, and Shaocong Ji. 2021. "A Hypogene Karst Development Pattern Controlled by the Deep-Cycle of Groundwater in the Syncline in Huanjiang, Guangxi, China" Water 13, no. 2: 199. https://doi.org/10.3390/w13020199
APA StyleDong, H., Dan, Y., Liang, J., Liang, B., Nie, G., & Ji, S. (2021). A Hypogene Karst Development Pattern Controlled by the Deep-Cycle of Groundwater in the Syncline in Huanjiang, Guangxi, China. Water, 13(2), 199. https://doi.org/10.3390/w13020199