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Nakanishi, Takahiro; Atarashi-Andoh, Mariko; Koarashi, Jun; Kokubu, Yoko; Hirai, Keizo*
Journal of Environmental Radioactivity, 128, p.27 - 32, 2014/02
Times Cited Count:7 Percentile:23.99(Environmental Sciences)Although considerable research has been conducted on the importance of recent litter versus older soil organic matter as DOC sources in forest soil, a more thorough evaluation of the temporal patterns of DOC and WEOC is necessary. We investigated the seasonal variation in water-extractable organic carbon in a Japanese cool-temperate beech forest soil by using the carbon isotopic composition (C and C) of WEOC as a tracer for the carbon sources. Fresh leaf litter DOC significantly contributed to WEOC in May when the snowmelt occurred. In the rainy season, increases in the concentration of WEOC and the proportion of hydrophobic compounds were caused by high microbial activity under wetter conditions. From summer to autumn, the WEOC in the mineral horizons was also dominated by microbial release from the soil organic matter. These results indicate that the origin and dynamics of WEOC are strongly controlled by seasonal changes in the environmental conditions.
Nakanishi, Takahiro; Atarashi-Andoh, Mariko; Koarashi, Jun; Kokubu, Yoko; Hirai, Keizo*
European Journal of Soil Science, 63(4), p.495 - 500, 2012/08
Times Cited Count:23 Percentile:61.86(Soil Science)To elucidate the origin and behavior of the water extractable organic carbon (WEOC), we first determined both the C andC of fractionated WEOC by DAX-8 resin in a cool-temperate beech forest soil. The enrichment of C in WEOC with depth reflected the increasing proportion of the hydrophilic (HPI) fraction to the hydrophobic acid (HPOA) fraction. The changes in C indicated that the major source of WEOC and its fractions was old organic matter in the mineral soil. Our results strengthened previous suggestion that the preferential adsorption of HPOA fraction and the preferential leaching of the indigenous soluble organic carbon in the mineral soils. This dynamic equilibrium between WEOC and the much greater soil organic carbon fraction plays an important role in carbon transport and accumulation throughout the soil profile.
Atarashi-Andoh, Mariko; Koarashi, Jun; Ishizuka, Shigehiro*; Hirai, Keizo*
Agricultural and Forest Meteorology, 152, p.149 - 158, 2012/01
Times Cited Count:33 Percentile:82.23(Agronomy)Radiocarbon (C) signature was used to partition soil respiration in a cool-temperate deciduous forest. Heterotrophic respiration strongly correlated with soil temperature, but the magnitude of the response to soil temperature was different between SOC decomposition and litter decomposition. Autotrophic respiration appeared to correlate strongly with the phenology index rather than soil temperature. The information on the seasonal change about the contribution ratio of each source to the soil respiration is essential to understand the intrinsic temperature sensitivity of each source and the other factors controlling soil respiration.
Atarashi-Andoh, Mariko; Koarashi, Jun; Ishizuka, Shigehiro*; Hirai, Keizo*
JAEA-Conf 2010-001, p.80 - 83, 2010/03
no abstracts in English
Atarashi-Andoh, Mariko; Koarashi, Jun; Ishizuka, Shigehiro*; Hirai, Keizo*
KURRI-KR-153, p.8 - 13, 2010/03
Soil organic carbon (SOC) is a complex of materials with different ages. An understanding of soil carbon cycling and thereby predicting its response to climatic change requires knowledge of both the inventory of carbon and the turnover times of SOC. In this study, chemical and density fractionation were examined to separate the organic matter collected from a beech forest into components with different turnover times. Mean residence time (MRT) for each fraction was estimated from its radiocarbon isotope ratio (C) using the C-MRT model. The results show that fractions separated by chemical fractionation with acid-alkali treatment have clearer difference in the isotope ratio than that by density fractionation. This means chemical fractionation is more adequate to estimate MRT composition for the beech forest soil. We also observed differences in the inventory and MRTs of carbon using chemical fractionation for two forests with different vegetation and the mean temperature. The results show that the difference in decomposed carbon flux from these two forests is attributed to the difference in MRT composition in each forest.
Koarashi, Jun; Atarashi-Andoh, Mariko; Ishizuka, Shigehiro*; Miura, Satoru*; Saito, Takeshi*; Hirai, Keizo*
Global Change Biology, 15(3), p.631 - 642, 2009/03
Times Cited Count:40 Percentile:74.36(Biodiversity Conservation)Although it is well documented the possibility that global warming can lead to an acceleration of microbial decomposition of soil organic carbon (SOC), the magnitude and timing of this effect remains highly uncertain. The main reason is a lack of quantitative aspect of the heterogeneity in SOC biodegradability. To quantify the heterogeneity, we collected the soil and litter samples within a cool-temperate deciduous forest in Japan, separated chemically the samples into SOC fractions, determined their mean residence times (MRTs) based on the radiocarbon (C) measurements, and finally represented the soil as a complex of six SOC pools with different range of MRTs. Predicted response of the SOC pools to warming demonstrates that the rate of SOC loss from the fast-cycling SOC pool diminishes quickly because of the substrate availability; in contrast, the warming continues to accelerate SOC loss from slow-cycling pools with MRTs of 20-200 year over the next century.
Atarashi-Andoh, Mariko; Koarashi, Jun; Ishizuka, Shigehiro*; Saito, Takeshi*; Hirai, Keizo*
JAEA-Conf 2008-003, p.75 - 78, 2008/04
C-14 is an effective tracer in investigating the carbon dynamics in the environment. In this study, the measurements of C-14 in soil organic matter (SOM) in a deciduous forest were used to determine the turnover time and CO production rate from SOM. In addition, monthly measurements of carbon isotopic ratios in soil-respired CO and atmospheric CO were conducted to characterize the seasonal variation of the contribution of each CO source, such as SOM decomposition and root respiration.
Koarashi, Jun; Atarashi-Andoh, Mariko; Ishizuka, Shigehiro*; Saito, Takeshi*; Hirai, Keizo*; Miura, Satoru*
Proceedings of International Symposium on Application of a Closed Experimental System to Modeling of C Transfer in the Environment, p.72 - 76, 2008/00
Recent debate has emphasized that our capacity to predict the response of soil organic carbon (SOC) to climate change depends on a clear understanding of the heterogeneity in SOC biodegradability. We collected soil samples from the Appi forest meteorology research site dominated by Japanese beech, separated the soil samples into three SOC fractions with a chemical method, and determined their radiocarbon isotope ratios using an accelerator mass spectrometry. The radiocarbon signatures allow us to estimate their turnover times (TTs), quantifying the rates of SOC decomposition. According to the estimated TTs, the SOC was distinguished into six SOC pools with distinct TTs of several years to 1000 years. The annual SOC decomposition rate was summed up to 0.47 kgC m y, about a half of which was from the fastest-cycling pool (litter). Approximately 5% of SOC gave the over-millennium TTs, suggesting that this pool plays a role of a long-term carbon sequestration in the carbon cycle.
Shimokawa, Tomoko*; Nakamura, Masaya*; Nagasawa, Naotsugu; Tamada, Masao; Ishihara, Mitsuro*
Shinrin Sogo Kenkyusho Kenkyu Hokoku, 6(1), p.27 - 34, 2007/03
The effect of -ray irradiation on enzymatic hydrolysis of spent enokitake mushroom substrate containing corncob meal and rice bran as major components was studied. Almost all the lignin component remained in the bottle though 34% of the original substrate was consumed. Polysaccharides consisting of glucose and xylose residues were the major components of the spent substrate. The saccharification rate of the spent substrate doubled with irradiation at a dose of 500 kGy, and the irradiated sample formed finer particles than the untreated sample after the same period of grinding. The holocellulose was apparently depolymerized by irradiation, resulted in the fragility of the substrate. An appreciable amount of xylan-derived sugars were extracted with water from the irradiated sample. The enzymatic saccharification rate of the irradiated spent enokitake substrate increased to over 80% with Cellulosin TP 25 from Trichoderma viride, which possesses endo--D-xylanase and -D-xylosidase activities as well as cellulase activities.
Ishii, Katsuaki*; Hosoi, Yoshihisa*; Hase, Yoshihiro; Tanaka, Atsushi
JAEA-Review 2006-042, JAEA Takasaki Annual Report 2005, P. 84, 2007/02
no abstracts in English
Koarashi, Jun; Atarashi-Andoh, Mariko; Miura, Satoru*; Saito, Takeshi*; Ishizuka, Shigehiro*
no journal, ,
no abstracts in English
Atarashi-Andoh, Mariko; Koarashi, Jun; Ishizuka, Shigehiro*; Saito, Takeshi*; Hirai, Keizo*
no journal, ,
Soil organic matter (SOM) is the major reservoir of carbon in terrestrial ecosystems. Thus, to evaluate the CO flux from SOM is an important step toward estimating the effect of environmental change on the terrestrial carbon cycles. In this study, we estimated the contribution of different soil CO sources (SOM, litter and root) to CO flux from the forest floor based on measures of carbon isotopic ratios in SOM, litter, soil-respired CO and atmospheric CO in a cool-temperate deciduous forest.
Koarashi, Jun; Atarashi-Andoh, Mariko; Ishizuka, Shigehiro*; Saito, Takeshi*; Hirai, Keizo*; Miura, Satoru*
no journal, ,
no abstracts in English
Koarashi, Jun; Atarashi-Andoh, Mariko; Ishizuka, Shigehiro*; Kadono, Atsunobu*; Moriya, Koichi*; Nakanishi, Takahiro
no journal, ,
Accelerated release of carbon (C) previously stored in soils is considered one of the most important positive feedbacks from terrestrial ecosystems to the atmosphere in a future warmer world. We used 14C analysis following chemical fractionation to quantify the sizes and turnover times of C pools of Japanese forest soils. The C-based approach revealed higher variations of the family of MRTs soil by soil. The size of C pools that cycle slowly on timescales of 100-1000 years strongly correlated with the content of pyrophosphate-extractable Al. In contrast, faster-cycling C pools that turn over within decades showed a negative correlation with mean annual temperature at the sites. Our results suggest that C dynamics in the isolated SOC pools may be regulated by different mechanisms: temperature control on decadal cycling C versus mineralogy control on slower-cycling C, and clearly demonstrate that the forest soils will respond very differently to climate change over the next century.
Koarashi, Jun; Atarashi-Andoh, Mariko; Ishizuka, Shigehiro*; Kadono, Atsunobu*; Moriya, Koichi*; Nakanishi, Takahiro
no journal, ,
Soils are the largest carbon (C) reservoir in terrestrial ecosystems, and may act as both a source and sink of atmospheric CO in response to climate change. Identifying the sizes and turnover times of soil organic carbon (SOC) pools is a crucial step to predicting the fate of soil C. Here, we used a C-based approach to quantitatively understand how much and how long Japanese forest soils store C in their surface horizons. We collected soil samples from deciduous forests, separated the samples into SOC fractions, and then determined their C ratios to estimate mean residence times (MRTs). The MRTs ranged from years to millennia, which revealed a different distribution of MRTs between the soils. We found that the total amount of C correlated positively with the size of the SOC pools cycling on time scales of 100 years, but poorly with the size of faster-cycling pools. The results suggest that the soils with higher C stocks do not necessarily have higher potential for CO emission.
Nakanishi, Takahiro; Koarashi, Jun; Atarashi-Andoh, Mariko; Hirai, Keizo*
no journal, ,
Dissolved organic carbon (DOC) is an important constituent in forest soils, because it affects soil formation and transport of heavy metals, is a source of C for microbes, and contributes to soil organic carbon (SOC) accumulation. In this study, we measured C and C in water extractable organic carbon (WEOC) to investigate the dynamics of DOC at Appi, a cool temperate deciduous forest in Japan. The C values of WEOC were slightly higher than those of SOC. Such enrichment in C indicated that WEOC production, which was coupled with the microbial activity, mainly used a C-enriched SOC fraction (including sugars, amino acids, etc.) of the total SOC. Indeed, hydrophilic fractions were enriched in C compared to the total WEOC. Hydrophilic fractions are considered more biologically available for decomposition. The result of C indicated that WEOC consists mainly of C-enriched, labile, hydrophilic organic materials with faster turnover times (several decades).
Moriya, Koichi*; Koarashi, Jun; Atarashi-Andoh, Mariko; Moriizumi, Jun*; Yamazawa, Hiromi*; Hirai, Keizo*
no journal, ,
Soil organic carbon (SOC) decomposition is an important component of the global carbon cycle, because SOC is the largest carbon reservoir in terrestrial ecosystems and a small change in the CO flux from SOC may lead to a large change in atmospheric CO concentration. For the accurate estimation of SOC decomposition, it is important to identify sizes and turnover times of SOC pools. We tried to estimate three SOC pools (active, slow and resistant) with different mean residence times (MRTs) by a combination of soil incubation and C analysis. The active SOC held 1% of the total SOC with MRTs of 1-3 weeks. The slow SOC accounted for 20-50% of the total with MRTs of 1 to 17 years. The active and slow SOC contributed greatly to the total CO production, and the primary source shifted from the active to the slow one. Our result shows the importance of quantifying the dynamics of rapidly-cycling SOC pools to accurately predicting the response of soils to climate change.
Atarashi-Andoh, Mariko; Koarashi, Jun; Moriya, Koichi; Nakanishi, Takahiro; Ishizuka, Shigehiro*; Hirai, Keizo*
no journal, ,
no abstracts in English
Moriya, Koichi; Koarashi, Jun; Atarashi-Andoh, Mariko; Moriizumi, Jun*; Yamazawa, Hiromi*; Ishizuka, Shigehiro*
no journal, ,
no abstracts in English
Moriya, Koichi; Koarashi, Jun; Atarashi-Andoh, Mariko; Moriizumi, Jun*; Yamazawa, Hiromi*; Ishizuka, Shigehiro*
no journal, ,
no abstracts in English