Rhizosphere Effects of Maize and Wheat Increase Soil Organic and Inorganic Carbon Release in Carbonate-Rich Soils: A Three-Source 13C Partitioning Study

Zhaoan Sun,Fanqiao Meng,Minyi He,Fang Wang,Biao Zhu

doi:10.3389/fenvs.2021.654354

Zhaoan Sun, Fanqiao Meng + Show 3 more

Open Access

https://doi.org/10.3389/fenvs.2021.654354

Copy DOI

Abstract

In carbonate-rich soils with plants, CO2 emissions from the rhizosphere may come from as many as three sources, that is, root-derived respiration, decomposition of soil organic carbon (SOC), and dissolution of soil inorganic carbon (SIC), so partitioning of CO2 emissions by source is important to accurately quantify the rhizosphere effect (RE). Because of limited methods for three-source partitioning of soil CO2, how living roots affect SOC and SIC release (RE) has not yet been clarified, and this urgently needs to be evaluated. In this study, the RE of summer maize and winter wheat on SOC decomposition and SIC dissolution was investigated at three phenological stages in pot experiments with the aid of 13CO2 pulse labeling combined with 13C natural abundance techniques. We found that the contribution of SIC dissolution to CO2 emissions from unplanted soils ranged from 25 to 44%. As crop growth progressed, the maize rhizosphere effect on SOC- and SIC-derived CO2 emissions increased from 14 and 74% at the elongation stage to 84 and 268% at the grain filling stage compared to that in unplanted soils, respectively, while the wheat rhizosphere effect on SOC- and SIC-derived CO2 emissions increased from 51 and 34% at the elongation stage to 77 and 76% at the grain filling stage. We concluded that the rhizosphere effects increased SOC and SIC release over the entire growing season of maize (by 54% for SOC and 159% for SIC) and wheat (by 64 and 49%) compared to those in unplanted soils, indicating that ignoring SIC dissolution in carbonate-rich soils with plants will result in overestimation of SOC decomposition.

Highlights

The soil carbon (C) pool comprises two components: soil organic C (SOC) and soil inorganic C (SIC)
The ratio of root/total maize significantly decreased from elongation until the grain filling stage (Figure 2C), while that of wheat showed no significant difference between elongation and anthesis and began to significantly decrease (Figure 2D)
Based on literature data from 13C/14C tracer experiments, we found that the contribution of root-derived CO2 to total soil CO2 emissions was 63% in maize-planted soil and 48% in wheat-planted soil (Figure 7C), which is comparable with our results (50% for maize and 42% for wheat; Figure 6)

Summary

Introduction

The soil carbon (C) pool comprises two components: soil organic C (SOC) and soil inorganic C (SIC). SIC is an important constituent in the carbonate-rich soils of arid and semiarid regions (Wang et al, 2014; Dong et al, 2019). Most of the studies on soil C emissions focused on SOC decomposition, but little attention was given to the role of SIC. Recent studies found that SIC can be considered a C source (carbonate dissolution and release; Zamanian et al, 2018; Liu et al, 2020) or C sink (secondary carbonate formation; Wang et al, 2014; Dong et al, 2019). The stability of the SIC pool directly affects atmospheric CO2 concentrations and the soil C balance

Methods

Results

Discussion

Conclusion