Congressional Research Service (CRS) report for Congress entitled “Entering the Executive Branch of Government: Potential Conflicts of Interest with Previous Employments and Affiliations” from 03/24/03.

Interview with African American North Texas State University alumnus James Gayle. The interview included Gayle's personal experiences of childhood, playing basketball at Fort Worth's all-black Terrell High School, attending North Texas and enrolling in the ROTC program, and his experience as a boarder in "Shack Town" neighborhood of Denton. Gayle talks about the comparison of race relations in Artesia, New Mexico, and Waco and Forth Worth, Texas, the "neutral" stance of NT administration toward black students and the "self-support" system among students, as well as his relationships with professors and white students, and his perception of what he gained from his NT experience.

Historically, attention on soil organic matter (SOM) has focused on the central role that it plays in ecosystem fertility and soil properties, but in the past two decades the role of soil organic carbon in moderating atmospheric CO{sub 2} concentrations has emerged as a critical research area. This chapter will focus on the storage and turnover of natural organic matter in soil (SOM), in the context of the global carbon cycle. Organic matter in soils is the largest carbon reservoir in rapid exchange with atmospheric CO{sub 2}, and is thus important as a potential source and sink of greenhouse gases over time scales of human concern (Fischlin and Gyalistras 1997). SOM is also an important human resource under active management in agricultural and range lands worldwide. Questions driving present research on the soil C cycle include: Are soils now acting as a net source or sink of carbon to the atmosphere? What role will soils play as a natural modulator or amplifier of climatic warming? How is C stabilized and sequestered, and what are effective management techniques to foster these processes? Answering these questions will require a mechanistic understanding of how and where C is stored in soils. The quantity …