The influence of rolled erosion control systems on soil temperature and surface albedo: Part I. A greenhouse experiment

✍ Scribed by R. A. Sutherland; T. Menard; J. L. Perry; D. C. Penn

• Publisher: John Wiley and Sons
• Year: 1998
• Tongue: English
• Weight: 847 KB
• Volume: 9
• Category: Article
• ISSN: 1085-3278
• DOI: 10.1002/(sici)1099-145x(199803/04)9:2<159::aid-ldr274>3.0.co;2-z

✦ Synopsis

A greenhouse study examined the in¯uences of various surface covers (a bare control soil and seven rolled erosion control systems ± RECS) on surface radiative properties, and soil temperature. In our companion paper we examine relationships with soil moisture, biomass production, and nutrient assimilation. Randomization and replication were key components to our study of microclimate under tropical radiation conditions. The bare Oxisol control soil exhibited the most extreme microclimatic conditions with the lowest albedo (not signi®cantly dierent from that of P300 1 North American Green, a dark green polypropylene system), and the highest mean and maximum hourly temperatures recorded at depths of 5 and 8 cm. This hostile climatic environment was not conducive to biomass production or moisture storage and it is likely that the observed soil surface crusts impeded plant emergence. Rolled erosion control systems, on the other hand, generally moderated soil temperatures by re¯ecting more shortwave radiation, implying less heat energy at the surface for conduction to the soil. The result was that RECS exhibited lower mean soil temperatures, higher minimum temperatures and lower maximum soil temperatures. An aspen excelsior system (Curlex I 1 Excelsior) had the highest albedo and the soil beneath this system exhibited the greatest temperature modulation. Open-weave systems composed of jute (Geojute 1 Price & Pictures) and coconut ®bers (BioD-Mat 70 1 RoLanka) were the RECS most similar in temperature response to the bare control soil. Other systems examined were intermediate in their temperature response and surface albedo (i.e.