ドローンカメラで乾燥地土壌の健全性を示す色素を測定(Drone cameras can measure pigments indicating surface health of drylands soils)

2026-07-29 ペンシルベニア州立大学(Penn State)

米ペンシルベニア州立大学(Penn State)の研究チームは、ドローン搭載カメラを用いて乾燥地域の土壌表面に生育する生物土壌クラスト(Biological Soil Crusts:BSC)の色素を遠隔測定し、土壌の健全性を評価できる手法を開発した。生物土壌クラストはシアノバクテリア、地衣類、コケなどから構成され、土壌の安定化、水分保持、炭素・窒素固定など乾燥地生態系に重要な役割を果たす。研究では、ドローン画像から光合成色素や保護色素の分布を高精度で推定できることを実証し、現地での採取や破壊的な分析を大幅に減らせることを示した。この技術により、生物土壌クラストの健全性や環境ストレスへの応答を広域かつ迅速に監視でき、気候変動や土地劣化、砂漠化の影響評価、乾燥地の保全・修復効果の検証に活用できると期待される。本成果は、リモートセンシングを活用した乾燥地環境の持続的モニタリング技術の発展に貢献するものである。

<関連情報>

高解像度マルチスペクトル画像を用いたシトネミン色素含有量と生物地殻機能指標のマッピング Mapping Scytonemin Pigment Content and Biocrust Functional Indicators Using High-Resolution Multispectral Imagery

Raúl Román, Tong Qiu, Fernando T. Maestre, Elizabeth A. La Rue, Sergio Vargas Zesati, Anthony Schaefer, Ryan V. Trexler, Nicole Pietrasiak, Estelle Couradeau
Remote Sensing in Ecology and Conservation  Published: 23 June 2026
DOI:https://doi.org/10.1002/rse2.70082

ドローンカメラで乾燥地土壌の健全性を示す色素を測定(Drone cameras can measure pigments indicating surface health of drylands soils)

ABSTRACT

Biocrusts are soil-surface assemblages of cryptogams, microbial communities, and soil particles, constituting the “living skin” of drylands. They are critical for global carbon and nitrogen cycles but are endangered by climate change. Safeguarding these critical components and their functions requires accurately measuring biocrust distribution and traits. Biocrust key functional indicators, such as pigments, provide information about their developmental stage, biomass, and functional state, but their remote quantification across spatial scales remains underdeveloped. We evaluated the potential of local-scale (tripod-acquired) multispectral imagery with machine learning to estimate pigments (scytonemin, chlorophyll a, carotenoids), soil organic carbon (SOC), and nitrogen (N) in two contrasting deserts: the Chihuahuan Desert (NM) and the Colorado Plateau (UT). High-resolution imagery (< 1 mm) alongside pigments and nutrient concentrations was collected. At NM site, support vector regressions (SVR) using blue and red bands achieved high accuracy for scytonemin (R2 = 0.93); red-edge band enhanced predictions for SOC and N (R2 = 0.95 and 0.80, respectively). In UT, predictive accuracy was lower (R2 < 0.6), likely due to scytonemin saturation. Scytonemin-based predictions of biocrust cover were less sensitive to moisture variability than chlorophyll a or carotenoids, suggesting scytonemin’s superiority as a biocrust index compared to previously developed indices. The best-performing local-scale models at the NM site successfully scaled to landscape-scale UAS imagery, allowing the remote prediction of pigments and nutrients and capturing relative differences associated with biocrust successional stages but did not capture the exact values of the modeled parameters compared to local measurements. The approach shows promise for future integration with satellite imagery to expand biocrust trait mapping at broader scales, offering a valuable tool for monitoring these key soil ecosystems and their functional attributes across diverse landscapes.

1902環境測定
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