@article {51168,
	title = {Controls of sediment transport capacity in laminar interrill flow on stone-covered surfaces},
	journal = {Water Resources Research},
	volume = {35},
	year = {1999},
	note = {//?//LTER III//},
	month = {1999},
	pages = {305-310},
	abstract = {<p>Sediment transport capacity is an important control on soil erosion and deposition by overland flow. To investigate the controls of transport capacity in laminar interrill overland flow on stone-covered surfaces, 357 flume experiments were performed using a single sediment size. Multiple regression analyses reveal that transport capacity is positively related to excess flow power ω - ω<sub><i>c</i></sub>, but the slope of the relation is steeper where ω \&lt; 0.3 W m<sup>-2</sup> than where ω >= 0.3 W m<sup>-2</sup>. Transport capacity is positively related to rainfall intensity where ω \&lt; 0.3 W m<sup>-2</sup> and negatively related to rainfall intensity where ω >= 0.3 W m<sup>-2</sup>. Transport capacity is negatively related to stone concentration and positively related to stone size irrespective of the value of ω. Finally, transport capacity is negatively related to fluid viscosity where ω \&lt; 0.3 W m<sup>-2</sup> and unrelated to viscosity where ω >= 0.3 W m<sup>-2</sup>.</p>
},
	keywords = {article, articles, hydrology, rills, hydrology, sediment transport, journal, journals},
	doi = {10.1029/98WR02534},
	url = {files/bibliography/JRN00271.pdf},
	author = {Gary Li and Athol D. Abrahams}
}
