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Hourly and daily rainfall intensification causes opposing effects on C and N emissions, storage, and leaching in dry and wet grasslands

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In this paper, the authors investigate the effects of expected twenty-first century changes in hourly and daily rainfall on soil carbon and nitrogen emissions, soil organic matter (SOM) stocks, and leaching using a coupled mechanistic soil biogeochemical model (BAMS2).
Abstract
Climate change is expected to alter hourly and daily rainfall regimes and, in turn, the dynamics of ecosystem processes controlling greenhouse gas emissions that affect climate. Here, we investigate the effects of expected twenty-first century changes in hourly and daily rainfall on soil carbon and nitrogen emissions, soil organic matter (SOM) stocks, and leaching using a coupled mechanistic carbon and nitrogen soil biogeochemical model (BAMS2). The model represents various abiotic and biotic processes involving 11 SOM pools. These processes include fungal depolymerization, heterotrophic bacterial mineralization, nitrification, denitrification, microbial mortality, necromass decomposition, microbial response to water stress, protection, aqueous advection and diffusion, aqueous complexation, and gaseous dissolution. Multi-decadal modeling with varying rainfall patterns was conducted on nine Australian grasslands in tropical, temperate, and semi-arid regions. Our results show that annual $${\text{CO}}_2$$ emissions in the semi-arid grasslands increase by more than 20% with a 20% increase in annual rainfall (with no changes in the rainfall timing), but the tropical grasslands have opposite trends. A 20% increase in annual rainfall also increases annual $${\text{N}}_2{\text{O}}$$ and NO emissions in the semi-arid grasslands by more than 10% but decreases emissions by at least 25% in the temperate grasslands. When subjected to low frequency and high magnitude daily rainfall events with unchanged annual totals, the semi-arid grasslands are the most sensitive, but changes in annual $${\text{CO}}_2$$ emissions and SOM stocks are less than $$5\%$$ . Intensification of hourly rainfall did not significantly alter $${\text{CO}}_2$$ emissions and SOM stocks but changed annual $${\text{NH}}_3$$ emissions in the tropical grasslands by more than 300%.

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Lawrence Berkeley National Laboratory
Recent Work
Title
Hourly and daily rainfall intensification causes opposing effects on C and N emissions,
storage, and leaching in dry and wet grasslands
Permalink
https://escholarship.org/uc/item/0zs3r5jb
Journal
Biogeochemistry, 144(2)
ISSN
0168-2563
Authors
Tang, FHM
Riley, WJ
Maggi, F
Publication Date
2019-07-30
DOI
10.1007/s10533-019-00580-7
Peer reviewed
eScholarship.org Powered by the California Digital Library
University of California

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&8'-+++1D-+;A:%

8%-+;-:/
$$&
82-+;A1B-+;5:
8E-+;F:7
&3&
&8C-++A1G
-+;61?-+;6:8G-++61(
-+;F:$82/*=<-+;A1
*-+;,:89
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5
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1
-++,1B-+;-:<7
&$$
C8(9:
7$
9(9
<<$
8(-++6:$8<-+;-:
9
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97
=/9
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$383
HBirch eectI*;4,F1#-+;+1J-+;+:(
$/7&
&&$
$$&9
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8(-+;F:
$$$
8B;4F6:$<$$8&/EK-+;-:
$8-+;5:$
8C-+;-:7&
/L7
$&//$
@$&
(9&
829:$82@:8#-+;F:9
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M7$
$$8**-+++:1
=2@
<$7
3&$
8*-+;-13*;4441

<C-++4:J
$&&
$$8E!-+;+1(
-+;F:&$$(9
<$$<$
$82?3-+;-:3$8##N-+;5:
8-+;6:8**-++,1(3
;44,:8#;44-1
(7;4F,1!-+++:$&
3&/
8-++F1((-++5:<
82?3-+;-:@L
$
$3$$&
97$
8#=;4441#-++5:$
$&&8C
-+;-1*-+;,:=
7&(9
&=/
&$

*%(;&!
8-+;5:&8-++F:$
&(9
O8*%(-1*%$(9
&-:;;(98&
:&$8$
77:3
$=
&=7
*%(-$3/$&
1
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991$1
3
7
&%
/

*%(-3

&$(9
*%(;$$!8-+;5:
&8-++F:O
38*%(-;:(98
:1&(9
8
:1&8
A
 
9
-
9
-
:1&$
8F
DEP
:$8B
HET
:/7<
$8B
AOB
:/7<$8B
NOB
:$
8B
DEN
:
@*%(- $(98!;O!F
;:%$$$
$&"F,&
8-+;5:@</8!4O
!;;:<$$
& 
$$F
DEP
B
HET
(97<$B
AOB
 
3$(9
*%(;8!-+;5:
$<$$
8(@$(;:
(8!;-O!;A:
8!;5O!;6:8-++F:
$$
$$8($(;:@
*%(-
-
7 8!;4:%!;4
$7
-
7$
7$
-
7$&
$=17$$
$$
8!-+;;:
C3$  8!-+O!-;:$&
8!-FO!-4"A,-++;1
%3;44A:$8!-67"

Citations
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Soil Organic Matter Research and Climate Change: Merely Re-storing Carbon Versus Restoring Soil Functions

TL;DR: In this paper, the authors argue that a far better strategy revolves around the effect of climate change on functions/services that soils render, since climatologists forecast less frequent but more intense rainfall events in the future, which may lead to food shortages, catastrophic flooding and soil erosion if soils are not able to cope.

Detection of spatially aggregated changes in temperature and precipitation extremes

TL;DR: In this article, the authors used a spatially aggregated perspective to detect a distinct intensification of heavy precipitation events and hot extremes and showed that much of the local to regional differences in trends of extremes can be explained by internal variability, which can regionally mask or amplify the forced long-term trends.
Journal ArticleDOI

Abiotic and Biotic Controls on Soil Organo–Mineral Interactions: Developing Model Structures to Analyze Why Soil Organic Matter Persists

TL;DR: In this article, the conundrum as to why some SOM decomposes rapidly, while other thermodynamically unstable SOM can persist on centennial time scales leads to substantial uncertainty in model structures, as well as uncertainty in the predictability of the land carbon sink trajectory.

Microbial Soil Respiration and its dependency on Carbon Inputs, Soil Temperature and Moisture in two contrasting ecosystems

TL;DR: In this article, three determinant factors in decomposition patterns of soil organic matter (SOM): temperature, water and carbon (C) inputs were studied. But the authors focused on the role of the above-defined environmental factors on the variability of soil C dynamics.
Journal ArticleDOI

Rainfall intensification increases the contribution of rewetting pulses to soil heterotrophic respiration

TL;DR: In this article, a stochastic model for soil heterotrophic respiration rates was developed, which analytically links the statistical properties of respiration to those of precipitation, and showed that both the mean rewetting pulse respiration and the mean respiration during drying increase with increasing mean precipitation.
References
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Journal ArticleDOI

Detection of spatially aggregated changes in temperature and precipitation extremes

TL;DR: In this article, the authors used a spatially aggregated perspective to detect a distinct intensification of heavy precipitation events and hot extremes and showed that much of the local to regional differences in trends of extremes can be explained by internal variability, which can regionally mask or amplify the forced long-term trends.
Journal ArticleDOI

Adsorption of ammonium by different natural clay minerals: Characterization, kinetics and adsorption isotherms

TL;DR: In this article, the NH4+ adsorption behavior followed the pseudo-second-order kinetic model for six natural clay minerals (NCM) evaluated for the effectiveness of NH4+, and the results showed that the NCM have significant potential as economic, safe and effective adsorbent materials for NH4 + adsorbing from the aqueous solution.
Journal ArticleDOI

Evidence of a strong coupling between root exudation, C and N availability, and stimulated SOM decomposition caused by rhizosphere priming effects.

TL;DR: In this paper, the authors provide quantitative evidence of a strong coupling between root exudation, SOM decomposition, and release of plant available N caused by rhizosphere priming effects.
Journal ArticleDOI

Soil respiration and human effects on global grasslands.

TL;DR: In this article, the authors quantify annual soil CO 2 efflux, contribution of root respiration to total soil respiration, apparent temperature sensitivity of soil oxygen, and turnover rates of soil organic carbon (SOC).
Journal ArticleDOI

Detection of continental-scale intensification of hourly rainfall extremes

TL;DR: In this article, the authors calculate continental-average changes in the magnitude and frequency of extreme hourly and daily rainfall observations from Australia over the years 1990-2013 and 1966-1989 and show that increases in daily rainfall extremes are consistent with CC scaling, but are within the range of natural variability.
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Q1. What are the contributions in "Hourly and daily rainfall intensification causes opposing effects on c and n emissions, storage, and leaching in dry and wet grasslands" ?

Here, the authors investigate the effects of expected twenty-first century changes in hourly and daily rainfall on soil carbon and nitrogen emissions, soil organic matter ( SOM ) stocks, and leaching using a coupled mechanistic carbon and nitrogen soil biogeochemical model ( BAMS2 ).