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Rural Development Policies and Sustainable Land Use in the ...

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34 CHAPTER 3<br />

Key socioeconomic elements of <strong>the</strong> survey<br />

at <strong>the</strong> household level <strong>in</strong>cluded household<br />

composition, education, asset ownership,<br />

labor use, sources of <strong>in</strong>come, sales of crop<br />

<strong>and</strong> livestock products, participation <strong>in</strong> credit<br />

markets, membership of organizations,<br />

participation <strong>in</strong> tra<strong>in</strong><strong>in</strong>g <strong>and</strong> extension programs,<br />

<strong>and</strong> collective action. Information<br />

collected at <strong>the</strong> parcel <strong>and</strong> plot levels <strong>in</strong>cluded<br />

l<strong>and</strong> tenure, cropp<strong>in</strong>g patterns, crop<br />

production, l<strong>and</strong> management technologies<br />

<strong>in</strong>clud<strong>in</strong>g use of labor <strong>and</strong> o<strong>the</strong>r <strong>in</strong>puts, <strong>and</strong><br />

conservation practices <strong>and</strong> <strong>in</strong>vestments.<br />

To be better able to analyze <strong>the</strong> adoption<br />

of conservation practices <strong>and</strong> suggest<br />

policies for susta<strong>in</strong>able l<strong>and</strong> use, <strong>the</strong> survey<br />

collected detailed biophysical data for a (r<strong>and</strong>omly<br />

drawn) sample of two plots on each<br />

farm. These <strong>in</strong>cluded l<strong>and</strong>scape attributes,<br />

plot size, type of soil parent material, erosion<br />

status, <strong>and</strong> presence of physical conservation<br />

structures. Soil samples were also<br />

taken <strong>and</strong> analyzed <strong>in</strong> a local soil laboratory<br />

<strong>and</strong> resulted <strong>in</strong> data regard<strong>in</strong>g pH, nutrient<br />

content, organic matter content, <strong>and</strong> texture.<br />

These data were used ma<strong>in</strong>ly for <strong>the</strong> calculation<br />

of soil moisture availability, 33 soil<br />

fertility, 34 <strong>and</strong> erosion risk. Soil fertility <strong>and</strong><br />

erosion risk served as a basis for <strong>the</strong> construction<br />

of a soil quality variable (Wielemaker<br />

2002). F<strong>in</strong>ally, <strong>the</strong> survey data were<br />

supplemented by add<strong>in</strong>g secondary <strong>in</strong>formation<br />

regard<strong>in</strong>g ra<strong>in</strong>fall, population density,<br />

market access, <strong>and</strong> road density. Most of<br />

<strong>the</strong>se data were obta<strong>in</strong>ed from CIAT.<br />

Econometric Analysis<br />

Ideally, we would like to estimate <strong>the</strong> system<br />

represented by equations (1)–(4) <strong>and</strong><br />

(6)–(8) us<strong>in</strong>g a systems approach such as<br />

three-stage least squares or full <strong>in</strong>formation<br />

maximum likelihood to deal with endogenous<br />

explanatory variables <strong>and</strong> account for<br />

correlation of error terms across <strong>the</strong> different<br />

equations. However, three-stage least<br />

squares estimation is not appropriate because<br />

<strong>the</strong>re are many limited dependent<br />

variables <strong>in</strong> this system, <strong>and</strong> jo<strong>in</strong>t maximum<br />

likelihood is not feasible due to <strong>the</strong><br />

large number of dependent variables <strong>and</strong><br />

error terms. Instead, we use s<strong>in</strong>gle-equation<br />

estimators appropriate to <strong>the</strong> nature of each<br />

dependent variable. L hpt<br />

are left-censored<br />

cont<strong>in</strong>uous variables (censored below at 0);<br />

hence we use a Tobit estimator to estimate<br />

equation (2). IN hpt<br />

, LM hpt<br />

, <strong>and</strong> P ht<br />

are dichotomous<br />

choice variables; we use probit<br />

models to estimate equations (3), (4), <strong>and</strong><br />

(7). LS ht<br />

is a polychotomous choice variable;<br />

we use a mult<strong>in</strong>omial logit model to<br />

estimate equation (6). y hpt<br />

<strong>and</strong> I ht<br />

are cont<strong>in</strong>uous<br />

uncensored variables; thus least squares<br />

regression is feasible <strong>and</strong> used for equations<br />

(1), (5), <strong>and</strong> (8).<br />

33<br />

Besides ra<strong>in</strong>fall, moisture availability <strong>in</strong> <strong>the</strong> soil is critical for crop growth <strong>and</strong> as such constitutes ano<strong>the</strong>r<br />

<strong>in</strong>dicator of agricultural potential. Moisture availability is soil specific <strong>and</strong> takes <strong>in</strong>to account not only ra<strong>in</strong>fall<br />

but also evapotranspiration, temperature, <strong>and</strong> soil characteristics. We used <strong>the</strong> data from our soil samples <strong>and</strong> operationalized<br />

moisture availability as crop water deficits for annual crops (for maize <strong>in</strong> <strong>the</strong> ma<strong>in</strong> <strong>and</strong> secondary<br />

grow<strong>in</strong>g seasons) <strong>and</strong> permanent crops (coffee). Water deficits were calculated on <strong>the</strong> basis of data for monthly<br />

temperature, effective ra<strong>in</strong>fall (tak<strong>in</strong>g runoff <strong>in</strong>to account as determ<strong>in</strong>ed ma<strong>in</strong>ly by slope, slope direction, contour<br />

curvature, profile curvature, <strong>and</strong> position on slope), evapotranspiration, <strong>and</strong> soil characteristics <strong>in</strong>clud<strong>in</strong>g depth,<br />

texture, <strong>and</strong> organic matter content. Only moisture availability for <strong>the</strong> second season was considered because <strong>the</strong><br />

data <strong>in</strong>dicated very few cases of ma<strong>in</strong> season water deficits. Moreover, moisture availability for coffee is highly<br />

correlated with moisture deficit for maize <strong>in</strong> <strong>the</strong> secondary grow<strong>in</strong>g season. For more details, see Wielemaker<br />

(2002).<br />

34<br />

Soil fertility is yet ano<strong>the</strong>r <strong>in</strong>dicator of agricultural potential. We approximated soil fertility by potential maize<br />

yield (nutrient-limited but not water-limited) us<strong>in</strong>g <strong>the</strong> QUEFTS (QUantitative Evaluation of soil Fertility <strong>and</strong> response<br />

To Fertilizers) model (Janssen 1990). For a given plot this model calculates potential yield on <strong>the</strong> basis of<br />

<strong>the</strong> soil’s nitrogen content, pH, <strong>and</strong> available potassium <strong>and</strong> phosphorus. We had data for each of <strong>the</strong>se variables<br />

from <strong>the</strong> analyses done <strong>in</strong> <strong>the</strong> soil laboratory of <strong>the</strong> FHIA (Honduras Foundation for Agricultural Research), a private<br />

agricultural research <strong>in</strong>stitute.

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