共 3 条
Comparing Two Different Development Methods of External Parameter Orthogonalization for Estimating Organic Carbon from Field-Moist Intact Soils by Reflectance Spectroscopy
被引:7
|作者:
Yu, Wu
[1
,2
]
Hong, Yongsheng
[2
,3
]
Chen, Songchao
[4
]
Chen, Yiyun
[3
,5
]
Zhou, Lianqing
[1
,2
]
机构:
[1] Tibet Agr & Anim Husb Univ, Coll Resource & Environm, Linzhi 860000, Peoples R China
[2] Zhejiang Univ, Coll Environm & Resource Sci, Inst Agr Remote Sensing & Informat Technol Applic, Hangzhou 310058, Peoples R China
[3] Wuhan Univ, Sch Resource & Environm Sci, Wuhan 430079, Peoples R China
[4] ZJU Hangzhou Global Sci & Technol Innovat Ctr, Hangzhou 311200, Peoples R China
[5] Chinese Acad Sci, State Key Lab Soil & Sustainable Agr, Nanjing 210008, Peoples R China
基金:
中国国家自然科学基金;
关键词:
visible and near-infrared spectroscopy;
soil organic carbon;
soil moisture;
external parameter orthogonalization;
local modeling;
NEAR-INFRARED SPECTROSCOPY;
LEAST-SQUARES REGRESSION;
SPECTRAL LIBRARY;
SEMIARID RANGELANDS;
SPATIAL VARIATION;
NIR SPECTROSCOPY;
CLIMATE-CHANGE;
EPO-PLS;
PREDICTION;
MATTER;
D O I:
10.3390/rs14061303
中图分类号:
X [环境科学、安全科学];
学科分类号:
08 ;
0830 ;
摘要:
Visible and near-infrared (Vis-NIR) spectroscopy can provide a rapid and inexpensive estimation for soil organic carbon (SOC). However, with respect to field in situ spectroscopy, external environmental factors likely degrade the model accuracy. Among these factors, moisture has the greatest effect on soil spectra. The external parameter orthogonalization (EPO) algorithm in combination with the Chinese soil spectroscopic database (Dataset A, 1566 samples) was investigated to eliminate the interference of the external parameters for SOC estimation. Two different methods of EPO development, namely, laboratory-rewetting archive soil samples and field-collecting actual moist samples, were compared to balance model performance and analytical cost. Memory-based learning (MBL), a local modeling technique, was introduced to compare with partial least square (PLS), a global modeling method. A total of 250 soil samples from Central China were collected. Of these samples, 120 dry ground samples (Dataset B) were rewetted to different moisture levels to develop EPO P1 matrix. Seventy samples (Dataset C) containing field-moist intact and laboratory dry ground soils were used to establish EPO P2 matrix. The remaining 60 samples (Dataset D) also containing field-moist intact and laboratory dry ground soils were employed to validate the spectral models developed based on Dataset A. Results showed that EPO could correct the effect of external factors on soil spectra. For PLS, the validation statistics were as follows: no correction, validation R-2 = 0.02; P1 correction, validation R-2 = 0.56; and P2 correction, validation R-2 = 0.57. For MBL, the validation results were as follows: no correction, validation R-2 = 0.06; P1 correction, validation R-2 = 0.65; and P2 correction, validation R-2 = 0.69. The P2 consistently yielded better results than P1 did but simultaneously increased the sampling time and economic cost. The use of the P1 matrix and the MBL algorithm was recommended because it could reduce the cost of establishing in situ models for SOC.
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页数:19
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