بدائل البحث:
step decrease » sizes decrease (توسيع البحث), we decrease (توسيع البحث)
teer decrease » greater decrease (توسيع البحث)
a decrease » _ decrease (توسيع البحث), _ decreased (توسيع البحث), _ decreases (توسيع البحث)
step decrease » sizes decrease (توسيع البحث), we decrease (توسيع البحث)
teer decrease » greater decrease (توسيع البحث)
a decrease » _ decrease (توسيع البحث), _ decreased (توسيع البحث), _ decreases (توسيع البحث)
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5121
S1 Data -
منشور في 2025"…Spatially, along the direction of groundwater flow, a general trend of increasing hydrochemical components was noted, with a significant rise in HCO<sub>3</sub>-Na type groundwater. (3) The spatiotemporal distribution and evolution of hydrochemistry were influenced by water-rock interactions, lithological characteristics, groundwater flow patterns, and human activities. …"
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5122
Groundwater contour map of the study area.
منشور في 2025"…Spatially, along the direction of groundwater flow, a general trend of increasing hydrochemical components was noted, with a significant rise in HCO<sub>3</sub>-Na type groundwater. (3) The spatiotemporal distribution and evolution of hydrochemistry were influenced by water-rock interactions, lithological characteristics, groundwater flow patterns, and human activities. …"
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5123
Endmember diagram of groundwater rock weathering.
منشور في 2025"…Spatially, along the direction of groundwater flow, a general trend of increasing hydrochemical components was noted, with a significant rise in HCO<sub>3</sub>-Na type groundwater. (3) The spatiotemporal distribution and evolution of hydrochemistry were influenced by water-rock interactions, lithological characteristics, groundwater flow patterns, and human activities. …"
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5124
The geological formation of the study area.
منشور في 2025"…Spatially, along the direction of groundwater flow, a general trend of increasing hydrochemical components was noted, with a significant rise in HCO<sub>3</sub>-Na type groundwater. (3) The spatiotemporal distribution and evolution of hydrochemistry were influenced by water-rock interactions, lithological characteristics, groundwater flow patterns, and human activities. …"
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5125
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5126
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5127
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5128
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5129
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5130
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5131
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5132
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5133
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5134
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5135
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5136
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5137
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5138
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5139
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5140