Abstract

This study was conducted to compare the methane (CH 4 ) production estimated by in vivo (sulfur hexafluoride tracer technique (SF 6 )) with that of two in vitro rumen simulation (RUSITEC) and gas production (IVGPT)) techniques. Four adult dry Holstein cows, aged 7.4±3.0 years and weighing 697±70 kg, were used for measuring methane production from five diets by the SF 6 technique. The experimental diets were alfalfa hay (D 1 ), corn silage + soybean meal (SBM) (910: 90, D 2 ), Italian rye grass hay +SBM (920: 80, D 3 ), rice straw +SBM (910: 90, D 4 ) and Sudan grass hay +SBM (920: 80, D 5 ). Each diet was individually fed to all 4 cows and 5 feeding studies of 17 d each were conducted to measure the methane production. In the RUSITEC, methane production was measured from triplicate vessels for each diet .In vitro gas production was measured for each of the diets in triplicate syringes. The gas produced after 24 and 48 h was recorded and gas samples were collected in vacuum vials and the methane production was calculated after correction for standard temperature and pressure (STP). Compared to the SF 6 technique, estimates of methane production using the RUSITEC were lower for all diets. Methane production estimated from 24 h in vitro gas production was higher (p<0.001) on D 1 as compared to that measured by SF 6 , whereas on D 2 to D 5 it was lower. Compared to SF 6 , methane production estimated from 48 h in vitro gas production was higher on all diets. However, methane estimated from the mean of the two measurement intervals (24+48 h/2) in IVGPT was very close to that of SF 6 (correlation 0.98), except on D 1 . The results of our study confirmed that IVGPT is reflective of in vivo conditions, so that it could be used to generate a database on methane production potential of various ruminant diets and to examine strategies to modify methane emissions by ruminants.

Highlights

  • Due to its low abundance in the atmosphere, the importance of methane on climatic impacts has often been undervalued in the past

  • Methane is one of the main greenhouse gases contributing to global warming with a 100-year global warming potential (GWP) 23 times that of carbon dioxide (CO2) (IPCC, 2001)

  • Many current inventories for enteric CH4 production are based on measurements of emission rates from ruminants in open circuit calorimeters under strictly controlled environments, with specific diets linked to energy balance (Murray et al, 1999)

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Summary

Introduction

Due to its low abundance in the atmosphere, the importance of methane on climatic impacts has often been undervalued in the past. Methane is one of the main greenhouse gases contributing to global warming with a 100-year global warming potential (GWP) 23 times that of carbon dioxide (CO2) (IPCC, 2001). Despite being present in the atmosphere at far lower concentrations than CO2, it is estimated that CH4 is responsible for approximately 20% of the greenhouse gas effect (IPCC, 2001). Accurate, yet simple, predictions of methane production of ruminants on any feeding regime are important in the nutrition of ruminants, and in modelling their contribution to methane emissions (Blummel et al, 2005). The correlation between methane outputs estimated in ruminants by respiration chamber and SF6 tracer technique is very high (Johnson et al, 1994). The SF6 technique involves the direct measurement of methane emissions from livestock.

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