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Household Demand for Water in Rural Kenya

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Abstract

To expand and maintain water supply infrastructure in rural regions of developing countries, planners and policymakers need better information on the preferences of households who might use the sources. Using data from 387 households in rural Kenya, we model source choice and water demand using a discrete-continuous (linked) demand model. We find that households are sensitive to the price, proximity, taste, and availability in choosing among sources, but are not sensitive to other source qualities including color, health risk, and risk of conflict. Estimates of the value of time implied by our model suggest that households value time spent collecting water at one third of unskilled wages. We use the linked demand framework to estimate own-price elasticities in the rural setting. These estimates range between − 0.13 and − 1.33, with a mean of − 0.56, and are consistent with other elasticity estimates from small and large cities.

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Notes

  1. A basic water service is a source within 30 min roundtrip of the household which, by nature of its design and construction, has the potential to deliver safe water (WHO/UNICEF 2017).

  2. Since our target sample was 400 households and the most recent census indicated a population of 3005 households in our study site, we targeted approximately 20% of the total population, or every fifth household. In 23 sampled households, the respondents in the household were unavailable so that call backs had to be scheduled. In 15 of these 23, an interview was later completed. Six households declined to be interviewed. Therefore, of the 402 households contacted, 387 were interviewed giving a response rate of 96%.

  3. Many households reported collecting from their “neighbor’s” well or private tap. Often these households reported walking significant distances to these “neighbors” and paying financial costs to collect, so we assume that many respondents were referring to the public sources just described.

  4. We do this for two reasons. First, the survey was conducted in the dry season and we have more confidence in respondents’ recall of water collection choices and trips when asked about the prior 7 days, rather than representative numbers for an “average week during the rainy season” several months prior. Second, many households collect rainwater in small containers during the rainy season and rely less on collection outside the home. Ninety-six percent of households collect rain water during the rainy season; the average household uses 230 l of rain water per week (during the rainy season). Although this seasonality is important for water supply planning, during the rainy season it is more difficult to observe households making the sorts of tradeoffs that help us identify their preferences.

  5. Based on the set of household-source pairs where we collected GPS locations as well as self-reported one-way walk times (we did not anticipate so many households to report collecting from their “neighbors”, and did not take GPS measurements at these sources), we estimate an implied walking speed of 1.7 miles per hour (results available on request). This is in line with other estimates (White et al. 1972; Calvo 1994; Tanser et al. 2006), suggesting the household’s self-reported walk times are plausible. We also calculate the difference in a household’s reported walk time to a given public source and their nearest neighbor’s reported walk time to the same source (we thank a referee for this suggestion). Among the 211 observations for which a household and their nearest neighbor reported having access to the same public source, the average difference (absolute value) in their reported walk times is 7.68 min (median: 2.91, SD 19.64). This represents on average a 12% difference in reported walk times between nearest neighbors (median: 5%), suggesting self-reported walk times are fairly precise.

  6. In practice, conditional demand equations have sometimes been misspecified in the water source choice and demand literature. Using either the Lee correction (Lee 1983) or Dubin-McFadden correction (Dubin and McFadden 1984) methods, analysts should estimate one conditional demand equation for each choice alternative (see original papers, or Mannering (1986), or Wu and Babcock (1998) for examples).

  7. Researchers in the recreational demand literature face similar issues. Here the discrete-continuous choices are which site to visit and how many visits to make. Suppose sites were fishing destinations, and the choice set included a salt-water site and three freshwater lakes. Data aggregation would collapse the choice set to a salt-water site and a freshwater lake, and fail to make use of any information on heterogeneity in lake characteristics like fish stocking, boat ramps, or water quality.

  8. We failed to achieve convergence when we allowed coefficients on the source type dummies to be random parameters.

  9. One explanation might be that perceived quality variables like taste, color and health risk are highly correlated, resulting in poor parameter estimates. We estimated several models that controlled for the modest correlation in our data (less than 0.5) between these quality variables. We also estimated models that added correlated quality variables one by one and in combinations. Finally, we estimated a model using a water quality index generated by principal component analysis. Results are generally consistent with our main model and are available upon request. Another concern might be that source-type dummies absorb the effects of quality attributes if there is little variation of quality attributes within source-types, though it is apparent from the raw results in Table 2 that there is substantial variation in source attributes within source-types.

  10. The reported coefficients for the random parameters logit are the mean of each individual parameter estimate. Note that the mean shadow value of walk time is given by \(60\times mean\bigg(\frac{{\hat{\psi }}_i^{walk}}{{\hat{\beta }}_i^{price}}\bigg)\) which is not the same as \(60\times \frac{mean({\hat{\psi }}_i^{walk})}{mean({\hat{\beta }}_i^{price })}\).

  11. The wealth index is calculated following Filmer et al. (2001) and Filmer and Scott (2012). It includes data on durable assets, electricity connection, sanitation, number of rooms, number of buildings, and main cooking fuel. More information on construction of the wealth index is available on request.

  12. \(E[{Pr_{ij}}\times {q_i}]=\hat{Pr_{ij}}\times \hat{q_i}\) if \(Cov({Pr_{ij}},{q_i})=0\). This can be tested empirically: in our sample we find \(Cov({Pr_{ij}},{q_i})=-0.05\), which is nominal compared to \(\hat{Pr_{ij}}\times \hat{q_i}\) (mean: 20.88).

  13. Since changes in attributes of sources not included in the household’s choice set are irrelevant to the household’s source choice and demand decision, these inequalities are not strict.

  14. \(\epsilon _j =\sum _{i=1}^{N}\bigg (\frac{\partial }{\partial P_{j}}\big (\hat{Pr_{ij}}\big )\times \hat{q_i}+\hat{Pr_{ij}}\times \frac{\partial }{\partial P_{j}}\big (\hat{q_i}\big )\bigg )\times \frac{P_{j}}{Q_j}=\sum _{i=1}^{N}\bigg (\beta _{i}^{price}Pr_{ij}\big (\eta Pr_{ij}+q_i(1-Pr_{ij})\big )\bigg )\times \frac{P_{j}}{Q_j}\)

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Acknowledgements

We thank Annalise Blum, Josephine Gatua, Mark Mwiti, and John Wainana for valuable assistance in the field and in data analysis. We also thank Dale Whittington, Celine Nauges, and two anonymous reviewers for helpful comments and suggestions. Funding for the project was provided by https://www.efdinitiative.org/kenya Environment for Development-Kenya with support from the Swedish International Development Cooperation Agency.

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Appendix: Materials

Appendix: Materials

See Tables 7, 8 and 9.

Table 7 First stage results for household demand model
Table 8 Correlation between average source attributes, and estimated own-price elasticity
Table 9 Correlation between average source attributes, and estimated own-price elasticity

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Wagner, J., Cook, J. & Kimuyu, P. Household Demand for Water in Rural Kenya. Environ Resource Econ 74, 1563–1584 (2019). https://doi.org/10.1007/s10640-019-00380-5

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