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  "notes": "The Mediterranean basin contains many semi-arid 
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environments where aquifers are subject to intensive exploitation, 
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environments where aquifers are subject to intensive exploitation, 
            
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generally to meet irrigation demands. The Campo de Cartagena aquifer 
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generally to meet irrigation demands. The Campo de Cartagena aquifer 
            
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is a clear example from such a semi-arid environment, and its 
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is a clear example from such a semi-arid environment, and its 
            
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hydrodynamic effects have aroused great scientific interest. The main 
110
hydrodynamic effects have aroused great scientific interest. The main 
            
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objective of this study is to evaluate the hydrodynamic effects that 
111
objective of this study is to evaluate the hydrodynamic effects that 
            
102
have occurred in the last century of anthropogenic activity in this 
112
have occurred in the last century of anthropogenic activity in this 
            
103
aquifer system. This aquifer is subject to intensive exploitation and 
113
aquifer system. This aquifer is subject to intensive exploitation and 
            
104
shows clear deficits in times of drought, with recharge by irrigation 
114
shows clear deficits in times of drought, with recharge by irrigation 
            
105
playing an important role. This study\u2019s methodology includes 
115
playing an important role. This study\u2019s methodology includes 
            
106
groundwater modelling to reconstruct the transient evolution of the 
116
groundwater modelling to reconstruct the transient evolution of the 
            
107
aquifer system during the last century, to generate water balances and 
117
aquifer system during the last century, to generate water balances and 
            
108
to illustrate how the evolution of irrigation has, in many ways, 
118
to illustrate how the evolution of irrigation has, in many ways, 
            
109
changed the aquifer\u2019s groundwater flow pattern. The results 
119
changed the aquifer\u2019s groundwater flow pattern. The results 
            
110
delineate the hydraulic communication of the aquifer stratums through 
120
delineate the hydraulic communication of the aquifer stratums through 
            
111
specific geological structures, as well as the flow transfer from the 
121
specific geological structures, as well as the flow transfer from the 
            
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Quaternary layer to the Mar Menor and the Mediterranean Sea. The 
122
Quaternary layer to the Mar Menor and the Mediterranean Sea. The 
            
113
reconstruction of the entire system\u2019s temporal evolution shows a 
123
reconstruction of the entire system\u2019s temporal evolution shows a 
            
114
fragile water balance that is supported by surface-water 
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fragile water balance that is supported by surface-water 
            
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contributions.",
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contributions.",
            
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    "es": "The Mediterranean basin contains many semi-arid 
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    "es": "The Mediterranean basin contains many semi-arid 
            
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environments where aquifers are subject to intensive exploitation, 
128
environments where aquifers are subject to intensive exploitation, 
            
119
generally to meet irrigation demands. The Campo de Cartagena aquifer 
129
generally to meet irrigation demands. The Campo de Cartagena aquifer 
            
120
is a clear example from such a semi-arid environment, and its 
130
is a clear example from such a semi-arid environment, and its 
            
121
hydrodynamic effects have aroused great scientific interest. The main 
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hydrodynamic effects have aroused great scientific interest. The main 
            
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objective of this study is to evaluate the hydrodynamic effects that 
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objective of this study is to evaluate the hydrodynamic effects that 
            
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have occurred in the last century of anthropogenic activity in this 
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have occurred in the last century of anthropogenic activity in this 
            
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aquifer system. This aquifer is subject to intensive exploitation and 
134
aquifer system. This aquifer is subject to intensive exploitation and 
            
125
shows clear deficits in times of drought, with recharge by irrigation 
135
shows clear deficits in times of drought, with recharge by irrigation 
            
126
playing an important role. This study\u2019s methodology includes 
136
playing an important role. This study\u2019s methodology includes 
            
127
groundwater modelling to reconstruct the transient evolution of the 
137
groundwater modelling to reconstruct the transient evolution of the 
            
128
aquifer system during the last century, to generate water balances and 
138
aquifer system during the last century, to generate water balances and 
            
129
to illustrate how the evolution of irrigation has, in many ways, 
139
to illustrate how the evolution of irrigation has, in many ways, 
            
130
changed the aquifer\u2019s groundwater flow pattern. The results 
140
changed the aquifer\u2019s groundwater flow pattern. The results 
            
131
delineate the hydraulic communication of the aquifer stratums through 
141
delineate the hydraulic communication of the aquifer stratums through 
            
132
specific geological structures, as well as the flow transfer from the 
142
specific geological structures, as well as the flow transfer from the 
            
133
Quaternary layer to the Mar Menor and the Mediterranean Sea. The 
143
Quaternary layer to the Mar Menor and the Mediterranean Sea. The 
            
134
reconstruction of the entire system\u2019s temporal evolution shows a 
144
reconstruction of the entire system\u2019s temporal evolution shows a 
            
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fragile water balance that is supported by surface-water 
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fragile water balance that is supported by surface-water 
            
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contributions."
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