Simultaneous Determination of Moisture, Organic Carbon, and Total Nitrogen by Near Infrared Reflectance Spectrophotometry

Ram C. Dalal, Robert J Henry

Soil Science Society of America Journal · 1986 · 550 citations · 0 references

Concepts

TL;DR

Near‑infrared diffuse reflectance spectrophotometry (NIR) was investigated for use in soil analysis. The study aimed to predict moisture, organic carbon, and total nitrogen contents simultaneously in air‑dried soils. An infraAlyzer 500 C spectrophotometer scanned soils at 2‑nm intervals, and calibration equations were derived by selecting the best combination of three wavelengths in a multiple regression analysis. The optimal wavelengths were 1926, 1954, and 2150 nm for moisture; 1744, 1870, and 2052 nm for organic carbon; and 1702, 1870, and 2052 nm for total nitrogen, yielding prediction errors of 0.58 %, 0.16 %, and 0.014 % for finely ground samples, though errors increased for coarsely ground soils, low‑organic‑matter soils, and those with wide color ranges, yet within a narrow color range and moderate organic matter the technique provides rapid, nondestructive simultaneous measurements.

Abstract

Abstract Near infrared diffuse reflectance spectrophotometry, within the wavelength range 1100 to 2500 nm, was investigated for use in the simultaneous prediction of the moisture, organic C, and total N contents of air‐dried soils. An infraAlyzer 500 C (Technicon Instruments Corp.) scanning spectrophotometer was used to obtain near infrared reflectance of soils at 2‐nm intervals. Calibration equations for each of the soil constituents studied were based upon selection of the best combination of three wavelengths in a multiple regression analysis. The wavelengths selected for moisture, organic C, and total N, respectively, were 1926, 1954, and 2150 nm, 1744, 1870 and 2052 nm, and 1702, 1870 and 2052 nm. The standard errors of prediction for finely ground samples (<0.25 mm) from the top layers (0‐0.1, 0.1‐0.2, 0.2‐0.3, 0.3‐0.6 m) were 0.58, 0.16, and 0.014% for moisture, organic C, and total N, respectively. The standard errors of prediction, however, were much larger for coarsely ground soils (<2 mm), soils containing low amounts of organic C (<0.3%) and total N (<0.03%), and for those with a wide range in colors. Within a narrow range in soil color and at moderate amounts of organic matter (0.3–2.5%C), the near infrared reflectance technique provides a rapid, nondestructive, and simultaneous measurement of moisture, organic C and total N in soils