Literature review of stemflow generation and chemical characteristics in Japanese forests

Ikawa, Reo

doi:10.4145/jahs.37.187

Cited by 9 publications

(7 citation statements)

References 38 publications

(29 reference statements)

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“…Mean throughfall inputs are reported to range from 27 to 96%, while canopy interception loss is reported to range from 9.7 to 19.5% in various deciduous forests (Price and Carlyle-Moses 2003). In Japan, the range of throughfall has been reported at 64-97% (Ikawa 2007). Throughfall above bamboo (88.4%) and canopy interception (11.6%) measured at this study site were within the ranges reported from other forests.…”

Section: Water Budgets and Dissolved Organic Carbon Flux During The Gsupporting

confidence: 63%

Dissolved organic carbon (DOC) input to the soil: DOC fluxes and their partitions during the growing season in a cool‐temperate broad‐leaved deciduous forest, central Japan

Chen

Yoshitake

Iimura

et al. 2017

Ecological Research

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Dissolved organic carbon (DOC) plays an important role in C cycling in forest ecosystems. Here we measured the concentrations and fluxes of DOC in a cool‐temperate broad‐leaved deciduous forest (Takayama Forest) to quantify the contribution of DOC from different forest water flux conditions. Mean DOC concentration during the growing season increased in the sequence from bulk precipitation (2.98 ± 0.45 mg L−1), throughfall above dwarf bamboo (6.84 ± 0.45 mg L−1), throughfall below dwarf bamboo (7.08 ± 0.42 mg L−1), stemflow (15.05 ± 0.98 mg L−1), and litter leachate (21.33 ± 1.01 mg L−1). Litter leachate DOC concentration, being high in spring and autumn, which was fairly correlated with the amount of litterfall of bamboo and trees. In stemflow, the DOC concentration was high during early summer and gradually decreased, in addition, it also showed dramatic variation among different plant species. Litter leachate (72.5%) accounted for most of the DOC input to the soil during the growing season (311.5 kg C ha−1 7 months−1), while stemflow (1.6%) contributed the least. A great quantity of precipitation at the study site was associated with a subsequent high atmospheric contribution of DOC flux (8.6%), which was more than half of throughfall (16.5%). The high input of DOC to the soil and andisol soil characteristics at the Takayama Forest suggest that the DOC fluxes are vital to the soil carbon sequestration. Therefore, DOC fluxes should be taken into account when the carbon balance is assessed at forest ecosystems.

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Section: Water Budgets and Dissolved Organic Carbon Flux During The Gsupporting

confidence: 63%

Dissolved organic carbon (DOC) input to the soil: DOC fluxes and their partitions during the growing season in a cool‐temperate broad‐leaved deciduous forest, central Japan

Chen

Yoshitake

Iimura

et al. 2017

Ecological Research

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“…Ikawa (2007) reported that percents of throughfall and stemflow to gross rainfall range between 64 and 97% and between 1 and 20%, respectively, in Japanese forests. Therefore, the values of this study are within the reported values.…”

Section: Discussionmentioning

confidence: 98%

A forest-structure-based analysis of rain flow into soil in a dense deciduous Betula ermanii forest with understory dwarf bamboo

2010

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The relationship between rain flow into the soil and forest structure was investigated in a dense deciduous Betula ermanii forest in northern Japan. The forest floor was covered with dwarf bamboo Sasa kurilensis. Observation was conducted from mid-July to late October in 1998. Leaf fall of Betula started in early September and ended in late October. Stemflow was proportional to rainfall and tree size [diameter at breast height (DBH)], and for the same rainfall, stemflow increased with leaf fall. On the contrary, throughfall decreased with leaf fall. Throughfall was intercepted also by Sasa in proportion to its leaf area. Multiple linear regression analysis revealed that stemflow and throughfall of Betula and Sasa were predictable as functions of rainfall and forest structural characteristics, such as DBH, tree density, and stand leaf mass. The rain interception by plants tended to decrease from summer to autumn, but the difference in the interception was about 2% between July (fully expanded leaves) and late October (lack of leaves). About 96 and 87% of rainfall reached the above-and below-Sasa layers, respectively. Thus, this study showed that understory Sasa is a major component of rain interception within the stand and that rain flow into the soil can be estimated by using rainfall and the forest structural parameters, such as DBH, tree density and stand leaf mass.

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“…Thirty-two years have passed since Parker [1983] published his literature review of throughfall and stemflow in the nutrient cycles of forests (see glossary for key terms, Appendix A) and 12 years since Levia and Frost [2003] published their review article on stemflow in the hydrologic and biogeochemical cycles of forested and agricultural ecosystems. Recognizing the complexity of water flux and the importance of stemflow in the hydrologic cycle of forests (Figure 1), another review specifically focusing on some stemflow studies in Japan was published by Ikawa [2007], while Johnson and Lehmann [2006] focused on the double funneling of stemflow above ground and below ground. In addition, Levia et al [2011a] reviewed some past throughfall and stemflow work and identified some future directions for stemflow research.…”

Section: Introductionmentioning

confidence: 99%

A review of stemflow generation dynamics and stemflow‐environment interactions in forests and shrublands

Levia

Germer

2015

Reviews of Geophysics

290

271

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Many geoscientists now recognize stemflow as an important phenomenon which can exert considerable effects on the hydrology, biogeochemistry, and ecology of wooded ecosystems and shrublands. Despite the explosive growth of stemflow research, until this review there has been no comprehensive attempt to summarize and synthesize this literature since 2003. Topical areas of substantive new knowledge in stemflow research include the following: (1) the interrelationships among stemflow and meteorological conditions, especially within individual rain events; (2) the dynamic interplay between stemflow and canopy structure; (3) stemflow and the cycling of solutes and transport of particulate matter; (4) stemflow and its interactions with canopy fungi and corticolous lichens; and (5) stemflow-soil interactions. Each of these five topical areas of substantive new stemflow research is summarized and synthesized, with areas of future research opportunities discussed. In addition, we have reviewed the parameters which can be used to describe stemflow and critically evaluate their utility for different purposes. This review makes a call for scientists studying stemflow to utilize common metrics in an effort to increase the cross-site comparability of stemflow studies. Capitalizing on the insights of prior research, exciting research opportunities await hydrologists, biogeoscientists, and forest ecologists who will conduct studies to deepen our knowledge of stemflow which will enable a better and more accurate framing of stemflow in the larger context of watershed hydrology and biogeochemistry.

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Literature review of stemflow generation and chemical characteristics in Japanese forests

Cited by 9 publications

References 38 publications

Dissolved organic carbon (DOC) input to the soil: DOC fluxes and their partitions during the growing season in a cool‐temperate broad‐leaved deciduous forest, central Japan

Dissolved organic carbon (DOC) input to the soil: DOC fluxes and their partitions during the growing season in a cool‐temperate broad‐leaved deciduous forest, central Japan

A forest-structure-based analysis of rain flow into soil in a dense deciduous Betula ermanii forest with understory dwarf bamboo

A review of stemflow generation dynamics and stemflow‐environment interactions in forests and shrublands

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