Factors are important elements in the siting process and affect the outcome of the site from different perspectives. A review of a large number of studies found that the selection of factors between dams showed certain similarities and characteristics, considering the differences that exist in the natural environment, social environment, and purpose. Analyzing the types and frequencies of factors in different articles can be useful in providing a reference for future site selection studies. It is essential to have advanced knowledge regarding the use of current study factors. For example, Othman [
19] analyzed the factors in different papers before making a decision on the selection of factors, and concluded that 70% used land use, soil type, slope, sedimentation, and CN grid; 20–40% used elevation, drainage networks, distance to lineaments, lithology, distance to faults, tectonic zone, distance to villages, distance to roads, and distance to towns; and less than 10% of the articles used distance to materials, total dissolved solids (TDS), evapotranspiration, and depression volume. Nevertheless, rainfall, slope, land-use, geological lithology, and soil type are all important factors in different siting scenarios.
4.1. Criteria for Dam Siting
In this section, the 39 site selection criteria from the 25 sample papers are assessed and grouped into six categories: hydrological, geological, topographical, water quality, environmental, and socioeconomic. The first five categories of factors belong to the broad range of environmental influences, while the last—socioeconomic—falls under the category of humanities and social sciences.
Table 4 presents the frequency with which different siting criteria were chosen. We also discuss the differences in criteria due to the various purposes of dams.
Topographic factors reflect important topographic features that directly determine whether a dam can find a suitable or optimal location. The slope and elevation rates are 88% and 56%. The hydrological factors characterize the potential for abundance or scarcity of water resources in the target area. Rainfall and runoff are cited with 32% probability and drainage network order with 28%, where runoff is a reflection of a fraction of the rainfall. Among the geological factors, geology/lithology is used at 68%. The rates of land use and soil type in environmental factors were 88% and 52%, respectively. The probability of water quality criteria as a weighting factor is low. Distance to roads was the most important in the economic community factors, with 32%. The quantitative analysis of the sample literature provides guidance for the selection of factors for future dam siting research. These factors are elaborated in the following sub-section.
4.1.1. Topographical Factors
Elevation and slope are the main criteria reflecting topographic characteristics. It is generally accepted that areas of moderate elevation are more suitable for dam construction, while lower and higher elevations show weak suitability [
19,
60]; however, researchers differ in their views on the suitability of steep versus moderate slopes for dam construction.
Othman [
19] argued that steepness is the main factor influencing dam siting, with smooth land being more suitable for dam construction than steep slopes, as did Buraihi [
85]. As the slope increases, so does the risk of landslides and the pressure on building foundations [
59,
86]. Ruzouq [
68] concluded that water velocity is proportional to slope, and that a slope of less than 5% has a positive effect on soil and water conservation in reservoirs, while Jha [
87] argued that the slope should be less than 15°. Groundwater dams are also chosen to be built on a gentle slope in wide valleys [
64]. On the other hand, Wimmer [
88] argued that excellent locations for dams are often found in canyons with steep slopes, where the topography can be used to the advantage of a shorter dam axis length and a larger capacity can be achieved with less construction earthwork, in agreement with Teschemacher [
89]. Jozaghi [
17] suggested that river valley shape is critical and that dams are preferable to be built at narrow locations where the upper river valley opens up, and that slope is generally greater at these locations. Becue [
90] relates valley morphology to dam site and types of dams. Natural structures with ideal river valley morphology are rare, so different dam types are fitted to different river valley morphologies. Wide valleys are suitable for earthfill dams, narrow sites for gravity dams, and even narrower sites for arch dams. The suitability of the slope is also closely related to the purpose of the dam: when used for rainwater harvesting, the Food and Agriculture Organization (FAO) recommends that the slope is no greater than 5% [
91]. In the siting of check dams, the slope determines the reservoir capacity and sedimentation, where a greater slope leads to greater sedimentation.
TWI describes the spatial pattern (location and size) of saturated areas affected by watershed-scale hydrologic processes, and characterizes the proportional relationship between moisture and contributing areas [
92]. TPI represents the difference between the raster and the mean elevation of the neighborhood (within the neighborhood), and is used to understand the relationship between runoff generation, flow rates, and sediment transport [
93,
94]. STI considers the influence of topography on erosion and clarifies the sediment transport potential to characterize erosion and sedimentation processes [
95]. SPI is used to quantify the erosive capacity of rivers, where the flow is a determinant of channel erosion and flood damage [
96]. TRI is one of the main factors affecting river potential energy, surface water storage capacity, runoff velocity, and river path at the watershed scale, characterizing elevation differences between adjacent raster [
97]. Rahmati [
98] proposed a check dam siting for soil and water conservation purposes, highlighting the importance of hydro-topographic factors and using five indices: TWI, TPI, STI, SPI, and TRI. Jamali [
64] used TWI to quantify the influence of hydrological processes by topography in groundwater siting in Pakistan.
Ildoromi [
99] chose three criteria in terrain characterization, in addition to slope, which are the most commonly used. Plan curvature and profile curvature were also used to express topographic features, which play an important role in embodying erosion and sedimentary geomorphology.
4.1.2. Hydrological Factors
Hydrological parameters determine the catchment capacity of the target area. The main hydrological factors include rainfall, runoff, catchment size, river network level, river network density, river width, and drainage network order. The statistics revealed that rainfall, runoff, river network class, and river network density were used more than 20% of the time, in order to provide reference for future studies.
Precipitation is the main source of runoff recharge, which has a positive impact on dam function when there are no natural disasters caused by extreme heavy precipitation events (e.g., landslides or floods). The runoff water quantity volume can be evaluated using the CSC-CN hydrologic process model [
100], or roughly estimated by the Hydrologic Analysis module of ArcGIS [
101]. The runoff curve number (CN) is an important tool for evaluating runoff volume. The CN value depends on soil type, land-use and land-cover, and hydrogeological conditions. The size of the catchment area is a prerequisite for determining the location of the dam. The catchment area should be large enough to maintain average reservoir storage, but not so large that the volume of water is often in excess of the reservoir capacity; otherwise, a more costly spillway would need to be built. The river network provides the essential runoff for the dams, and different river network classes indicate different runoff volumes when the rivers are upstream tributaries and downstream mainstems. River network density reflects the water resources in the region, and a higher river network density shows better diversion capacity in the face of floods, while river network density and flood volume show a positive correlation trend [
98]. The river network rank indirectly reflects the runoff volume, where higher-order rivers have higher runoff volume.
4.1.3. Geological Factors
The geological conditions of the dam site are critical and directly affect the safety and stability of the project. The geological foundation of the site also affects the dam type [
102] and dam construction materials [
86,
103]. The site should have impermeable geology, dam foundation, and no leakage; for example, southwest China is a typical karst landscape region, and the lithology directly affects whether the water will “leak away” after the dam is built [
104]. Geological-related indicators include geology/lithology, tectonic zones, distance to faults, and distance to lineaments.
Lithology is the most important geological factor [
17], which was used 68% of the time, with which the influence of faults and tectonic lines are considered. Different epochs form ground rock units representing different conditions of stability and degreez of pressure resistance [
19]. Karst areas, due to the karst phenomenon of carbonate rocks, have been observed in China, where the construction of underground dams in karst areas has led to excessive groundwater siltation which, in turn, has led to flooding in the upstream lowlands [
105]. Therefore, the construction of underground dams needs to consider the water retention capacity of karst areas and the complexity of the underground routes of caves. Faulting is one of the main factors causing landslides [
106]; thus, the farther the site is from a fault, the lower the risk of landslides. Unstable tectonic zones and lineaments also have potential risks.
While 60–70% of the analyzed papers chose 1 or 2 geological factors, Othman [
19] chose four geological factors: tectonic zones, lithology, distance to lineaments, and distance to faults. Less suitable tectonic zones include the Imbricated Zone and the High Folded Zone, where faults and lineaments represent geological weaknesses and are usually avoided by buffer zones.
4.1.4. Environmental Factors
The environment is a broad concept. In this case, we chose environmental factors including soil environment (soil type, erosion), land-use, distance to water resources, and groundwater resources. However, this is obviously not representative of all environmental criteria, and are only common environmental factors used in the sample literature. The two criteria of land-use and soil type had the highest usage rates: 88% and 52%, respectively.
Soil types can be classified according to soil texture, which leads to different rates of soil infiltration and, thus, different effects on the runoff volume. Sufficiently water-resistant fine-grained foundations, clays, and clay mixtures are recommended [
102,
107]. High population activity, increased construction, and deforestation are the main causes of soil erosion [
108,
109,
110], and increased erosion in the watershed has a direct impact on the accumulation of sediment in the reservoir, making areas of soil erosion less suitable for dams intended for water storage. Land-cover reveals land-use patterns, as well as links to current social development. Changes in land-use and vegetation usually affect the water cycle [
111]. Furthermore, the different land-use types can be quickly filtered, in order to identify areas suitable for development and use. The distance to water resources reflects the connection to the river network in that watershed and, if the dam is still some distance from the river, then water resources may become the biggest problem facing it.
4.1.5. Water Quality Factors
Water quality criteria are mostly considered for the siting of groundwater dams, which determine the quality and drinking safety of groundwater resources for development and utilization, however, surface dams for irrigation or water supply purposes are among those that use water quality factors.
Jozaghi [
17] proposed indicators of salinity and sodium levels of water bodies to limit the water quality conditions used for agricultural irrigation: TDS, SSP, PH, and EC. These indicators are related to agricultural needs, such as soil suitability for cultivation, infiltration rate, and plant growth suitability. Ruzouq [
68] also used the TDS to characterize the quality of water in a study area located in the Arabian Gulf, where the high salinity of the water is the main problem that must be overcome and avoided.
4.1.6. Socioeconomic Factors
Different social settings manifest as differences in socioeconomic criteria for siting. Closeness to roads and settlements, leading to lower transportation costs, had a 32% usage rate. Distance to material facilities, roads, cities, and villages are used to quantify construction cost issues. Distance to the countryside and distance to the city are two different situations, which usually require a certain distance from the city but being as close to the countryside as possible. This is because rural areas can bring the required labor force, while dams are not suitable within a certain buffer zone within the city, in order to prevent large accidents such as dam failures [
112].
Othman [
19] chose the distances from the city, the countryside, and the road to weigh the optimal solution, in terms of economic cost. Emamgholi [
106] presented unique social factors—the welfare, culture, and participation of the residents in the actual work—and conducted field investigations. Dam construction has an impact on the nearby residents, and the support of local residents determines the smoothness of the project.
4.2. The Influence of Dam Use on Criteria Selection
The objectives of decision makers vary widely, making it difficult to generalize a number of criteria for dam siting. Decision factors vary by purpose of the dam, from large hydroelectric power generation dams (e.g., the world-leading Three Gorges Dam) to small dams for irrigation and aquaculture.
Lempérière [
113] considered the dams of the future as being multipurpose, while Abushandi [
63] identified five major purposes of modern hydraulic facilities: regulation and flood control under an extremely uneven spatial distribution of water resources, soil erosion and sediment control, drought control, irrigation, and hydropower generation. According to the latest data from the ICOLD 2020 statistics (
Table 6) [
16], irrigation is the major purpose, accounting for 47% and 24% of the sole-purpose and multiple-purpose statistics of dams, respectively. The next three major purposes are hydropower, water supply, and flood control.
The purpose determines the siting of different water collection structures and hydraulic facilities, such as retention basins, reservoirs, check dams, and rainwater harvesting structures (RWH), in order to achieve the spatial regulation of water resources. Check dams are built on seasonal streams, in order to intercept runoff from catchment-contributing areas and store it to optimize water utilization. RWH are important technologies for storing fresh water or recharging groundwater resources, for purposes such as water supply and agricultural irrigation. Singh [
114] pointed out the differences between four types of catchment structures—RWH, check dams, percolation tanks, and farm ponds—in the process of determining sites (
Table 7).
In order to clarify the link between the siting factors and purposes of dams, information was collated from 25 sample papers, selected for the four main types of dam purposes: irrigation, hydropower, water supply, and flood control.
Table 8 reflects the frequencies (in percentage) of criteria used in different types of dams, where the total percentages of sub-criteria under each type of criteria in the four types of uses is 100%.
The preferred factors in topography are slope and elevation, which highly influence the construction of irrigation, hydropower, and flood control dams, and which together account for 21%, 23%, and 19% of these three types of uses, respectively. Runoff and rainfall are important hydrological factors, which are more important in irrigation, water supply, and flood control, accounting for 17%, 12%, and 15% respectively. Geological factors are significantly more prominent in hydropower dams than for the other three purposes, up to 22%. The most important of the environmental factors are land-use and soil type, with higher percentages for irrigation and water supply, accounting for 30% and 15% respectively. Water quality indicators are concentrated in dam siting studies for water supply and irrigation purposes, hydropower and flood control types of dams are usually not involved in water quality standards. Finally, socioeconomic factors maintained relative importance in all purposes.
In the irrigation of crops and domestic water supply, water quality standards are important factors in the siting of surface and underground dams and rainwater harvesting structures [
17,
115]. To ensure crop safety and food security, water quality standards are important factors in dams for irrigation and water supply purposes. Poor water quality can negatively affect crop productivity, crop quality, and the public health of consumers and farmers, who are in direct contact with the irrigation water [
116]. Globally, at least 20 million hectares of agricultural land are irrigated with treated or untreated wastewater [
117], often containing excess sodium, magnesium, chloride, and boron, which affect soil alkalinity, phytotoxicity, and heavy metal content. However, geological factors play a dominant role in underground dams for such purposes, including sub-factors such as geological lithology, distance to faults, and distance to lineaments [
118,
119,
120].
Hydroelectric power plants are dams designed to generate electricity by impounding rivers and converting the kinetic and potential energy of water into electrical energy using hydraulic turbines. According to the ICOLD, there will be 6115 dams for the purpose of power generation by 2020, of which 4135 will be multi-purpose dams [
16]. The Three Gorges Dam, one of the world’s 10 largest dams, is a multi-purpose dam that not only provides a huge supply of electricity, but also provides excellent flood control [
121]. The hydrological index [
122], installed hydroelectric capacity [
123], and potential power generation [
124] are the main considerations in the siting design of hydropower dams. Rojanamon [
125] proposed four directions of consideration for the siting factors of power stations—engineering, economic, environmental standards, and social impacts—and integrated the sub-factors of each direction, using GIS analysis to process to obtain the best potential siting area. Jafar [
126], on the other hand, based on GIS and combined with the best-worst method (BWM) in MCDM, determined the optimal location model for hydropower dams, in terms of four aspects: physical, environmental, socioeconomic, and technological.
Floods and other water-related disasters account for 70% of all deaths associated with natural hazards [
127], and flood control is one of the most important elements of sustainable water resource management [
128]. Flood control dams can largely mitigate the catastrophic effects of floods. There are 2539 sole-purpose flood control dams and 4911 multi-purpose flood control dams worldwide [
16]. In Egypt, which suffers from frequent seasonal flooding and droughts, as well as water demand for agricultural irrigation, the Aswan Dam largely regulates the extremely uneven distribution of water resources and achieves spatial and temporal deployment of the multi-year runoff from the Nile [
129]. The critical factors for the siting of flood control dams include the design height of the dam, which is limited by topographic conditions, hydrological characteristics, and technology, where the height of the dam directly affects the possibility of flooding and, indirectly, the possibility of dam failure [
130]. Sumi [
131] also pointed out that the relationship between dam height and storage capacity varies greatly between countries, due to differences in geographic conditions; for example, the ratio of storage capacity to dam height is particularly large for dams in the United States, as these dams are often built in gently sloping rivers and wide river valleys. Patel [
132] considered the good soil and water conservation functions of check dams to moderate flooding and soil erosion in small watersheds.