Modelling the benefits of soil water conservation using the PARCH model - a case study from a semi-arid region of Kenya

Citation
W. Stephens et Tm. Hess, Modelling the benefits of soil water conservation using the PARCH model - a case study from a semi-arid region of Kenya, J ARID ENV, 41(3), 1999, pp. 335-344
Citations number
11
Categorie Soggetti
Environment/Ecology
Journal title
JOURNAL OF ARID ENVIRONMENTS
ISSN journal
01401963 → ACNP
Volume
41
Issue
3
Year of publication
1999
Pages
335 - 344
Database
ISI
SICI code
0140-1963(199903)41:3<335:MTBOSW>2.0.ZU;2-A
Abstract
Field experiments in the semi-arid regions of Kenya have shown that soil wa ter conservation techniques can result in increased maize grain yields. The degree of benefit in a particular season is dependant on the rainfall amou nt and distribution. However, the results of field experiments are limited to a few years of observations at specific locations and it is therefore di fficult to make generalized conclusions about the benefits in years of diff ering rainfall patterns. The PARCH model has been calibrated for Katumani Composite 'B'-a local vari ety of maize used in the Machakos district of Kenya-and validated against o bserved grain and dry matter yields from experimental plots. Historical dai ly rainfall data were collected for Katumani Research Station, in the semi- arid region of Kenya, during the period 1961 to 1994. Seasonal totals for t he short rains (October to February) and long rains (February to August) we re calculated and nine years were selected as representative of 'wet','aver age' and 'dry' seasons for the long and short rains, respectively. The PARCH model was then used to simulate the maize grain yield under three soil water conservation scenarios: (i) a typical situation where 30% of ra infall above a 15 mm threshold is lost as runoff, (ii) runoff control, wher e all rainfall infiltrates, and (iii) runoff harvesting, which results in 6 0% extra 'rainfall' for rains above 15 mm. The soil was taken to be a sandy clay loam which is typically found in the region. Two planting densities o f 4 4 and 8.8 plants m(-2) were used to simulate normal and high levels of management. Planting dates were determined from the 30% runoff scenario and were fixed for the other scenarios to avoid confounding the results. The results showed that runoff control and runoff harvesting produce signif icant yield increases in 'average' years in both the long rains and the sho rt rains. However, in 'dry' years there were only small yield increases in the short rains and negligible benefit in the long rains. In 'wet' years th ere were no significant yield increases due to water conservation in either season. Clearly, these results are a simplification of the real situation where wat er conservation strategies may allow earlier planting or be accompanied by increased planting densities, both of which may result in yield increases. However, this work demonstrates the usefulness of appropriate crop growth m odels in evaluating a wider range of crop management strategies under a rea listic range of climatic conditions than would be possible in the field. (C ) 1999 Academic Press.