Water resources
Across the Texas High Plains, thousands of irrigation wells pump the Ogallala Aquifer faster than rain refills it; along the Gulf Coast and in Florida some wells are starting to yield salt water. The fresh water available is tiny compared with all the water on the planet, and almost all of what we use is hidden underground.
Distribution and the hydrological cycle
Three kinds of water. Surface water flows or sits on the land (rivers, lakes, reservoirs): the Colorado River supplies cities and farms across the Southwest. Groundwater fills the pores of rock and sediment: the Ogallala Aquifer irrigates crops across the Great Plains. Atmospheric water is vapor, clouds and fog; people use it mainly after it falls as rain, though fog nets collect small amounts in dry places.
What approximate percentage of Earth's water is salt water? Where is most fresh water concentrated?
What approximate percentage of Earth's water is salt water? Where is most fresh water concentrated?
Distinguish between surface water, groundwater, and atmospheric water, and give an example of human use of each.
Distinguish between surface water, groundwater, and atmospheric water, and give an example of human use of each.
What is the water cycle? Name its main processes and explain which energy drives it.
What is the water cycle? Name its main processes and explain which energy drives it.
What is surface runoff and which terrain factors (slope, vegetation, permeability) increase or reduce it?
What is surface runoff and which terrain factors (slope, vegetation, permeability) increase or reduce it?
The graph shows the distribution of water on Earth. River and lake water (marked with '?') represents $1.2\ \%$ of fresh water. Calculate what percentage of total…
The graph shows the distribution of water on Earth. River and lake water (marked with '?') represents $1.2\ \%$ of fresh water. Calculate what percentage of total planetary water this represents and comment on what this figure implies for managing the resource.
In a drainage basin of $150\ \text{km}^2$, the historical average annual water balance was: precipitation $P = 750\ \text{mm/year}$, actual evapotranspiration…
In a drainage basin of $150\ \text{km}^2$, the historical average annual water balance was: precipitation $P = 750\ \text{mm/year}$, actual evapotranspiration $ETR = 450\ \text{mm/year}$, effective infiltration into the aquifer $I = 150\ \text{mm/year}$, and surface runoff $Es = 150\ \text{mm/year}$. Over the last three decades, $35\ \%$ of the basin's surface area has been sealed by industrial parks and housing developments.
- a) State the water balance equation ($P = ETR + Es + I \pm \Delta S$) and predict qualitatively and semi-quantitatively how the terms $Es$ and $I$ will change. Picture and explain how the flood hydrograph of the main river will change (basin response time and peak flow) during a flash flood event of $80\ \text{mm}$ in $4\ \text{h}$.
- b) Climate change projections predict a $15\ \%$ decrease in annual precipitation and an increase in average temperature of $+1.8\ ^\circ\text{C}$ (increase in potential evapotranspiration). Explain why a $15\ \%$ reduction in rainfall does not cause an equivalent $15\ \%$ drop in streamflow, but rather a proportionally much greater decrease in available runoff.
- c) Design two actions based on Sustainable Drainage Systems (SuDS) that can be integrated into the urban fabric of the basin to restore the original infiltration values and mitigate flood risk.
Groundwater
Springs and seasons. A spring flows where the water table meets the land surface. In the wet season recharge lifts the water table above the outlet and the spring flows; in the dry season the water table drops below the outlet and the spring stops. Comal Springs in Texas flows from the Edwards Aquifer, and its flow falls when the aquifer is low.
Discharge wetlands. Where the water table reaches the surface, groundwater seeps out and feeds ponds, lagoons and streams, as in Florida's springs and wetlands. Pumping from nearby wells creates a cone of depression: the water table dips around each well. Even if nobody pumps from the wetland itself, it loses its inflow, and many wells together can lower the whole water table.
Artificial recharge. People add water to an aquifer on purpose. Infiltration ponds spread water over permeable soil so it seeps down; injection wells pump it straight into the aquifer. Orange County, California, recharges its aquifer with highly treated wastewater. It is most useful where overpumping has lowered the water table or seawater is moving inland: injection wells along the coast build a freshwater barrier.
What is an aquifer and what rock properties (porosity, permeability) make it possible?
What is an aquifer and what rock properties (porosity, permeability) make it possible?
What is the water table and which factors, such as recharge by rainfall or pumping, make it rise or fall throughout the year?
What is the water table and which factors, such as recharge by rainfall or pumping, make it rise or fall throughout the year?
Distinguish between an unconfined aquifer and a confined aquifer. Which of the two can give artesian wells and why?
Distinguish between an unconfined aquifer and a confined aquifer. Which of the two can give artesian wells and why?
What is a spring and what relationship does it have with an aquifer? Explain why some springs only flow in the wet season.
What is a spring and what relationship does it have with an aquifer? Explain why some springs only flow in the wet season.
According to Darcy's law, groundwater flows faster through gravels than through clays. Explain that law qualitatively (hydraulic gradient and permeability) and its…
According to Darcy's law, groundwater flows faster through gravels than through clays. Explain that law qualitatively (hydraulic gradient and permeability) and its practical consequence when choosing where to drill a well.
What is artificial aquifer recharge and which techniques are used (infiltration ponds, injection wells)? In which situations of overexploitation or saltwater intrusion…
What is artificial aquifer recharge and which techniques are used (infiltration ponds, injection wells)? In which situations of overexploitation or saltwater intrusion is it especially useful?
Agricultural nitrates can take decades to disappear from an aquifer even if fertilization is reduced. Explain the concept of residence time of groundwater and its…
Agricultural nitrates can take decades to disappear from an aquifer even if fertilization is reduced. Explain the concept of residence time of groundwater and its implications for the recovery of polluted aquifers.
In the aeolian mantle and marshes of Doñana, the Almonte-Marismas aquifer system sustains peridunal lagoon complexes of high ecological value and discharges freshwater…
In the aeolian mantle and marshes of Doñana, the Almonte-Marismas aquifer system sustains peridunal lagoon complexes of high ecological value and discharges freshwater into the tributary streams that feed the marsh.
- a) Explain the hydrogeological functioning of a peridunal lagoon (such as Santa Olalla) as a discharge wetland connected to the water table, and predict how the hydrological dynamics of the basin respond when massive pumping for red berry cultivation creates cones of depression in the vicinity, even if water is not pumped directly from the lagoon.
- b) In the hydrogeological monitoring network, it is observed that several streams have shifted their regime from gaining (effluent) to losing (influent) reaches, and that former artesian wells on the edge of the marsh have ceased to flow spontaneously. Interpret both facts in terms of hydraulic gradients and piezometric pressures in the confined and semi-confined levels.
- c) Faced with the degradation of the wetland, two proposals clash: constructing a surface water transfer from another basin to maintain the current irrigated area versus shutting down illegal wells and purchasing agricultural estates for their renaturalization. Argue which of the two solutions guarantees long-term sustainability based on ecosystem resilience and the ecological limits of the resource.
Overexploitation and saltwater intrusion
A Mediterranean hydrographic basin experiences a continuous dry cycle over five years. The evolution recorded by the river basin authority is as follows: Year 1:…
A Mediterranean hydrographic basin experiences a continuous dry cycle over five years. The evolution recorded by the river basin authority is as follows:
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Year 1: Rainfall decreases by $30\ \%$ compared to the average; reservoirs are at $65\ \%$ and the rainfed crop yield remains acceptable.
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Year 2: Rainfall scarcity persists; soil moisture drops drastically and $80\ \%$ of the rainfed cereal crop is lost, although the main river continues to flow thanks to groundwater discharges from a karst aquifer.
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Year 3: Reservoirs drop below $20\ \%$, springs and fountains dry up, and the state government urgently authorizes the opening of "drought wells" in the headwater aquifers to save irrigated farming.
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Years 4 and 5: Rainfall normalizes ($100\ \%$ of the average), but piezometric levels do not recover, springs remain dry, and several wells experience ground subsidence problems.
- a) Chronologically identify in which years meteorological drought, agricultural drought, and hydrological drought manifest, justifying the time lag and inertia that exist between them.
- b) Explain from a hydrogeological perspective why the aquifers were able to buffer the streamflow in Year 2, but suffered hysteresis and mechanical damage (such as the compaction of aquitard formations and irreversible loss of porosity) after the intensive exploitation of Year 3.
- c) Design a technical protocol for activating drought wells: establish three rigorous quantitative indicators (piezometric thresholds, water electrical conductivity, and environmental base flow) that must be strictly met to immediately suspend emergency pumping.
Water treatment and management
Drinking water treatment, stage by stage. (1) Intake with screens removes sticks and debris. (2) Coagulation–flocculation: a chemical such as alum makes tiny suspended particles clump into larger flocs. (3) Settling: the heavy flocs sink and are removed. (4) Filtration through sand and gravel removes the remaining fine particles and some microbes. (5) Chlorination kills disease-causing microbes and leaves a little chlorine in the pipes. The EPA sets the limits under the Safe Drinking Water Act.
Wastewater treatment. Primary treatment uses screens and settling to remove solids. In secondary treatment, activated sludge works like this: air is bubbled into the wastewater so microorganisms eat the dissolved organic matter, and then the microbes settle out as sludge. The test is BOD (biochemical oxygen demand): the oxygen, in mg/L, that microbes use up in 5 days. High BOD means lots of organic matter, and a good plant cuts BOD by about 90% or more. Tertiary treatment removes nutrients and disinfects.
Desalination. In reverse osmosis, pressure higher than the water's osmotic pressure pushes seawater through a membrane that holds back the salts. It has two big costs: energy (pumping at very high pressure) and brine, a waste stream much saltier than seawater that can harm marine life if it is dumped carelessly. Carlsbad, California, runs the largest US plant, which supplies a large part of San Diego County's water (the exercise's "southeastern Spain" can be read as southern California). Large volumes are often given in $\text{hm}^3$ in exercises: $1\ \text{hm}^3 = 10^6\ \text{m}^3 = 0.001\ \text{km}^3$, and $1\ \text{hm}^3 \approx 811$ acre-feet. A "state water agency" or "river basin authority" is just the agency that manages the basin, such as a state water board or the Bureau of Reclamation.
Reading water-quality data. Dissolved oxygen (DO): low values mean trouble for fish. BOD and COD (chemical oxygen demand): high values mean organic pollution. Nitrate: from fertilizer and sewage, and it feeds algae blooms. Conductivity: more dissolved salts. Fecal coliforms: sewage contamination. A sewage discharge raises BOD, COD, nitrate and coliforms and drops DO, because microbes use up the oxygen; farther downstream the river slowly cleans itself.
Drought types. A drought moves through stages. Meteorological: rainfall below average. Agricultural: soil moisture drops and rainfed crops fail. Hydrological: rivers, reservoirs and aquifers run low; rivers fed by groundwater keep flowing at first. Socioeconomic: shortages, restrictions and economic losses.
Allocation in shortage. When reserves cannot meet all demands, drinking water and basic human needs come first, then the minimum flow that keeps the river ecosystem alive, then farms and industry. Among crops, perennial orchards usually rank above annual crops, since losing trees means losing years of production. In the US West, water rights often follow first in time, first in right, as on the Colorado River.
Transfers and alternatives. A transfer sends water from one basin to another (like the California Aqueduct). It takes flow from the donor river, so the lower reach and mouth get less water, more salt moves into the estuary, less sediment and fewer nutrients arrive, and fish and wetlands suffer, mainly in the dry season. Volumes are often given in acre-feet in the US: $1\ \text{acre-foot} \approx 1{,}233\ \text{m}^3$ (in SI, $1\ \text{km}^3 = 10^9\ \text{m}^3$). Desalination powered by solar energy avoids lowering rivers, but it costs more and makes brine.
The efficiency paradox (Jevons paradox). Drip irrigation cuts the water lost per acre, but farmers often use the savings to irrigate more land or thirstier crops, so total pumping can go up. Also, water lost by flood irrigation often seeps back into the aquifer, while the water that evaporates or is transpired (consumptive use) is gone for good. Efficiency alone does not fix a deficit; caps on total withdrawals do.
Put the stages of a drinking water treatment plant in order: filtration, intake, settling, chlorination, and coagulation-flocculation. Explain what is removed in each…
Put the stages of a drinking water treatment plant in order: filtration, intake, settling, chlorination, and coagulation-flocculation. Explain what is removed in each stage.
A wastewater treatment plant with secondary treatment uses activated sludge with microorganisms. Explain what this biological treatment consists of and which parameter…
A wastewater treatment plant with secondary treatment uses activated sludge with microorganisms. Explain what this biological treatment consists of and which parameter (BOD) is used to verify its effectiveness.
What is the water footprint of a product? Compare that of wheat, avocado and a kilogram of beef, and explain what debate is raised by exporting "water-rich" products…
What is the water footprint of a product? Compare that of wheat, avocado and a kilogram of beef, and explain what debate is raised by exporting "water-rich" products from dry regions.
Reverse osmosis desalination plants supply a large part of south-eastern Spain. Explain the principle of the process and assess its two great costs: energy consumption…
Reverse osmosis desalination plants supply a large part of south-eastern Spain. Explain the principle of the process and assess its two great costs: energy consumption and brine management.
A Mediterranean coastal region with intensive early-season agriculture and mass tourism requests an annual water transfer of $150\ \text{hm}^3$ from an Atlantic basin…
A Mediterranean coastal region with intensive early-season agriculture and mass tourism requests an annual water transfer of $150\ \text{hm}^3$ from an Atlantic basin whose reservoirs are at $48\ \%$ of their capacity. As a technical alternative, the state water agency proposes the construction of two reverse osmosis desalination plants powered by an annexed solar photovoltaic plant.
- a) Analyze the hydrogeological and ecological impacts that the continuous withdrawal of flows would cause in the lower reach and the mouth of the donor basin, considering the seasonal variability of the Atlantic river regime.
- b) Evaluate the technical and environmental feasibility of desalination as an alternative in the receiving area: predict two specific environmental impacts of desalination plants (brine discharge management and energy balance) and justify why the unit cost of desalinated water usually generates opposition among irrigators compared to transferred water.
- c) Refute with ecological and hydrological arguments the statement by the farmers' association: "River water that flows into the sea is a lost and wasted resource if it is not transferred."
A semi-arid inland basin has renewable water resources of $60\ \text{hm}^3/\text{year}$, compared to a licensed demand of $75\ \text{hm}^3/\text{year}$, of which…
A semi-arid inland basin has renewable water resources of $60\ \text{hm}^3/\text{year}$, compared to a licensed demand of $75\ \text{hm}^3/\text{year}$, of which $80\ \%$ corresponds to traditional flood irrigation. To tackle the deficit, the state water agency financed the comprehensive modernization to drip irrigation, achieving a theoretical reduction in plot consumption of $30\ \%$. However, after the work, the overexploitation of the underlying aquifer has worsened.
- a) Explain the "efficiency paradox" (rebound effect or Jevons paradox) applied to irrigation: justify how the reduction of irrigation return flows to the aquifer and farmers' decisions (switching to more profitable crops and expanding irrigated acreage) contribute to the worsening of the overall water balance.
- b) The regional wastewater treatment plant (WWTP) produces $6\ \text{hm}^3/\text{year}$ of secondary-treated effluent, with an electrical conductivity of $2\,900\ \mu\text{S/cm}$ and $28\ \text{mg/L}$ of nitrates. Evaluate the agronomic (phytotoxicity, soil salinization) and environmental risks of its direct use in irrigation, and deduce what tertiary treatments or blending schemes are mandatory before its application.
- c) Design the main guidelines of a water rights and permit revision plan that allows reaching quantitative balance in the basin, justifying what environmental and socioeconomic criteria should guide the reductions.
A river monitoring station tracks the physical-chemical and biological water quality at four points along a river during low-flow conditions: Point 1 (forested…
A river monitoring station tracks the physical-chemical and biological water quality at four points along a river during low-flow conditions:
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Point 1 (forested headwater): $\text{OD} = 9.4\ \text{mg/L}$; $\text{DBO}_5 = 1.2\ \text{mg/L}$; $\text{DQO} = 3.0\ \text{mg/L}$; $\text{NO}_3^- = 3.5\ \text{mg/L}$; Conductivity $= 180\ \mu\text{S/cm}$; Fecal coliforms $= 15\ \text{CFU}/100\ \text{mL}$.
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Point 2 (downstream of an urban discharge without adequate treatment): $\text{OD} = 1.8\ \text{mg/L}$; $\text{DBO}_5 = 70\ \text{mg/L}$; $\text{DQO} = 115\ \text{mg/L}$; $\text{NO}_3^- = 14\ \text{mg/L}$; Conductivity $= 820\ \mu\text{S/cm}$; Fecal coliforms $= 95\,000\ \text{CFU}/100\ \text{mL}$.
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Point 3 ($20\ \text{km}$ downstream, after an extensive intensive irrigated floodplain with mineral fertilization): $\text{OD} = 6.0\ \text{mg/L}$; $\text{DBO}_5 = 6\ \text{mg/L}$; $\text{DQO} = 16\ \text{mg/L}$; $\text{NO}_3^- = 72\ \text{mg/L}$; Conductivity $= 2\,200\ \mu\text{S/cm}$; Fecal coliforms $= 350\ \text{CFU}/100\ \text{mL}$.
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Point 4 (downstream of a petrochemical and industrial park with prior physical-chemical treatment): $\text{OD} = 4.2\ \text{mg/L}$; $\text{DBO}_5 = 10\ \text{mg/L}$; $\text{DQO} = 160\ \text{mg/L}$; $\text{NO}_3^- = 11\ \text{mg/L}$; Conductivity $= 3\,100\ \mu\text{S/cm}$; Fecal coliforms $= 200\ \text{CFU}/100\ \text{mL}$.
- a) Interpret the biodegradability of the discharges by comparing the $\text{DBO}_5/\text{DQO}$ ratio at points 2 and 4. Justify what causes the critical drop in dissolved oxygen at point 2 using the conceptual model of river self-purification.
- b) Diagnose the origin of the pollution at point 3 by analyzing the nitrate and conductivity values. Assess the consequences on the aquatic macroinvertebrate community and explain whether this water is suitable for withdrawal for human consumption without prior denitrification.
- c) Design the necessary treatment stages in the wastewater treatment plant responsible for the discharge at P2, and two structural corrective measures in the agricultural practices at P3 to restore the parameters within ecological limits.
In a river basin with regulating reservoirs, stored reserves at the beginning of the water year are only $180\ \text{hm}^3$ due to an exceptional drought. The annual…
In a river basin with regulating reservoirs, stored reserves at the beginning of the water year are only $180\ \text{hm}^3$ due to an exceptional drought. The annual water-right demands under normal conditions are:
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Urban water supply for a metropolitan area of $1.2$ million inhabitants: $80\ \text{hm}^3$.
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Irrigation of perennial woody crops (irrigated olive groves and citrus fruits): $90\ \text{hm}^3$.
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Irrigation of annual herbaceous crops (corn and rice): $70\ \text{hm}^3$.
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Cooling of a thermal power plant and chemical industry: $20\ \text{hm}^3$.
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Environmental reserve flow in the main river: $40\ \text{hm}^3/\text{year}$ (continuous $1.27\ \text{m}^3/\text{s}$ to prevent the degradation of the estuary).
- a) The irrigators' association demands the complete suspension of the environmental flow during the drought, arguing that "the law places agriculture ahead of fish, and the river can always recover later." Technically rebut this statement by explaining why the environmental flow is not just another consumptive use, but a prior restriction that conditions all other uses according to the Clean Water Act and state water law.
- b) Design a justified proposal for allocating and restricting the $180\ \text{hm}^3$ among the different sectors, applying the legal order of priority of uses and justifying the reduction percentage assigned to each.
- c) Justify agronomically and economically why, within the agricultural sector, the water volume reduction must be applied asymmetrically, prioritizing survival irrigation for woody crops over annual herbaceous crops.
Back to the start: on the High Plains, pumping the Ogallala faster than it recharges lowers the water table and dries up wells and springs; on the Gulf Coast and in Florida, overexploitation causes saltwater intrusion and salinizes the wells.