Abstract

Cover crop system has shown a potential approach to improving carbon sequestration and environmental quality. Six of each winter and summer cover crops were subsequently grown in two soils, Krome gravelly loam soil (KGL), and Quincy fine sandy soil (QFS), in phytotrons at 3 temperatures (10/20, 15/25, 25/30oC for winter/summer cover crops) to investigate their contributions for carbon (C) sequestration. Among winter cover crops, the highest and the lowest amounts of C accumulated were by bellbean (Vicia faba L.), 597 g/m2 and white clover (Trifolium repens), 149 g/m2, respectively, in the QFS soil. Among summer cover crops, sunn hemp (Crotalaria juncea L.) accumulated the largest quantity of C (481 g/m2), while that by castorbean (Ricinus communis) was 102 g/m2 at 30oC in the KGL soil. The mean net C remained in the residues following the 127 d decomposition were 187 g/m2 of C (73% of the total) and 91 g/m2 (52% of the total) for the winter and summer cover crops, respectively. Following a whole cycle of winter and summer cover crops grown, the mean soil organic C (SOC) increased by 13.8 and 39.1% in the KGL and QFS soil, respectively, compared to the respective soils before. The results suggest that triticale, ryegrass, and bellbean are the promising winter cover crops in the QFS soil, while sunn hemp, velvetbean (Mucuna pruriens), and sorghum sudangrass (Sorghum bicolor × S. bicolor) are recommended summer cover crops for both soils under favorable temperatures.

Highlights

  • Soil carbon (C) sequestration by terrestrial vegetation, as one of the main approaches for greenhouse gas (GHG) mitigation, has long been identified by the Intergovernmental Panel on Climate Change [1]

  • The results suggest that triticale, ryegrass, and bellbean are the promising winter cover crops in the Quincy fine sandy soil (QFS) soil, while sunn hemp, velvetbean (Mucuna pruriens), and sorghum sudangrass (Sorghum bicolor × S. bicolor) are recommended summer cover crops for both soils under favorable temperatures

  • The soil type had no significant influence on the above parameters for the summer cover crops, while in the case of winter cover crops, it significantly influenced the biomass production and the total N

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Summary

Introduction

Soil carbon (C) sequestration by terrestrial vegetation, as one of the main approaches for greenhouse gas (GHG) mitigation, has long been identified by the Intergovernmental Panel on Climate Change [1]. Soil is the largest terrestrial C pool, constitutes at 2500 Pg of total C (organic and inorganic) within one meter depth [4]. This soil C pool is approximately two-thirds of the total C in ecosystems [5]. The former is about 3.3-fold greater than the atmospheric C pool (760 Pg), and 4.5-fold greater than the biotic C pool (560 Pg) [6]. Soil organic carbon (SOC) pools have the slowest turnover rates in general terrestrial ecosystems [7], C sequestrated in soils has a great potential to mitigate CO2 emission to the atmosphere [3]

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