Klute, A. (1986) Water Retention: Laboratory Methods. In: Methods of Soil Analysis: Part 1—Physical and Mineralogical Methods, ASA and SSSA, Madison, 635-662.
https://doi.org/10.2136/sssabookser5.1.2ed.c26

has been cited by the following article:

• TITLE: Temperature Sensitivity of Nitrogen Dynamics of Agricultural Soils of the United States

  AUTHORS: Amitava Chatterjee, Alexsandro Felipe de Jesus, Diksha Goyal, Sailesh Sigdel, Larry J. Cihacek, Bhupinder S. Farmaha, Sindhu Jagadamma, Lakesh Sharma, Daniel S. Long

  KEYWORDS: Arrhenius Equation, Soil Organic Carbon, Inorganic Nitrogen, Gaseous Losses of Nitrogen

  JOURNAL NAME: Open Journal of Soil Science, Vol.10 No.7, July 30, 2020

  ABSTRACT: Soil temperature controls gaseous nitrogen losses through nitrous oxide (N2O) and ammonia (NH3) fluxes. Eight surface soils from agricultural fields across the United States were incubated at 10°C, 20°C, and 30°C, and N2O and NH3 flux were measured twice a week for 91 and 47 d, respectively. Changes in cumulative N2O and NH3 flux and net N mineralization at three temperatures were fitted to calculate Q10 using the Arrhenius equation. For the majority of soils, Q10 values for the N2O loss ranged between 0.23 and 2.14, except for Blackville, North Carolina (11.4) and Jackson, Tennessee (10.1). For NH3 flux, Q10 values ranged from 0.63 (Frenchville, Maine) to 1.24 (North Bend, Nebraska). Net soil N mineralization-Q10 ranged from 0.96 to 1.00. Distribution of soil organic carbon and total soil N can explain the variability of Q10 for N2O loss. Understanding the Q10 variability of soil N dynamics will help us to predict the N loss.