光谱学与光谱分析
光譜學與光譜分析
광보학여광보분석
SPECTROSCOPY AND SPECTRAL ANALYSIS
2015年
8期
2113-2118
,共6页
郑小坡%孙越君%秦其明%任华忠%高中灵%吴伶%孟庆野%王金梁%王建华
鄭小坡%孫越君%秦其明%任華忠%高中靈%吳伶%孟慶野%王金樑%王建華
정소파%손월군%진기명%임화충%고중령%오령%맹경야%왕금량%왕건화
高光谱遥感%可见光-短波红外%土壤水分%定量反演%NSSAI
高光譜遙感%可見光-短波紅外%土壤水分%定量反縯%NSSAI
고광보요감%가견광-단파홍외%토양수분%정량반연%NSSAI
Hyperspectral remote sensing%VIS-SWIR%Soil moisture%Quantitative inversion%NSSAI
土壤是地表能够生长植物的疏松土层。它由不同矿物质、有机物质、空气、水分、微生物等组成,其中土壤含水量变化较大,利用遥感技术快速准确的反演土壤含水量具有重要意义。针对反演土壤含水量受土壤类型影响较大的问题,提出构建归一化光谱斜率吸收指数(normalized spectral slope and absorption index ,NSSAI),用于削弱土壤类型对土壤水分反演影响。其建模方法如下:首先在野外采取不同类型的土壤样本,制备不同土壤含水量的土样,利用ASD光谱仪采集不同含水量下的土壤反射率光谱,然后根据各类土壤在不同含水量下的光谱响应规律,提取短波红外水分的光谱吸收特征和可见光波段的土壤光谱斜率,综合两者在降低土壤类型影响土壤含水量反演精度的各自优势,构建归一化光谱斜率吸收指数,进一步建立该指数与土壤含水量之间的线性拟合关系来计算土壤含水量。实验结果表明,与传统利用单一土壤水分光谱吸收特征参数及其变形的方法相比,基于NSSAI构建的土壤含水量反演模型拟合精度较高(相关系数为0.93),在土壤含水量较低和较高的情况下都能有效排除土壤类型差异造成的影响,提高了裸土土壤含水量的反演精度。
土壤是地錶能夠生長植物的疏鬆土層。它由不同礦物質、有機物質、空氣、水分、微生物等組成,其中土壤含水量變化較大,利用遙感技術快速準確的反縯土壤含水量具有重要意義。針對反縯土壤含水量受土壤類型影響較大的問題,提齣構建歸一化光譜斜率吸收指數(normalized spectral slope and absorption index ,NSSAI),用于削弱土壤類型對土壤水分反縯影響。其建模方法如下:首先在野外採取不同類型的土壤樣本,製備不同土壤含水量的土樣,利用ASD光譜儀採集不同含水量下的土壤反射率光譜,然後根據各類土壤在不同含水量下的光譜響應規律,提取短波紅外水分的光譜吸收特徵和可見光波段的土壤光譜斜率,綜閤兩者在降低土壤類型影響土壤含水量反縯精度的各自優勢,構建歸一化光譜斜率吸收指數,進一步建立該指數與土壤含水量之間的線性擬閤關繫來計算土壤含水量。實驗結果錶明,與傳統利用單一土壤水分光譜吸收特徵參數及其變形的方法相比,基于NSSAI構建的土壤含水量反縯模型擬閤精度較高(相關繫數為0.93),在土壤含水量較低和較高的情況下都能有效排除土壤類型差異造成的影響,提高瞭裸土土壤含水量的反縯精度。
토양시지표능구생장식물적소송토층。타유불동광물질、유궤물질、공기、수분、미생물등조성,기중토양함수량변화교대,이용요감기술쾌속준학적반연토양함수량구유중요의의。침대반연토양함수량수토양류형영향교대적문제,제출구건귀일화광보사솔흡수지수(normalized spectral slope and absorption index ,NSSAI),용우삭약토양류형대토양수분반연영향。기건모방법여하:수선재야외채취불동류형적토양양본,제비불동토양함수량적토양,이용ASD광보의채집불동함수량하적토양반사솔광보,연후근거각류토양재불동함수량하적광보향응규률,제취단파홍외수분적광보흡수특정화가견광파단적토양광보사솔,종합량자재강저토양류형영향토양함수량반연정도적각자우세,구건귀일화광보사솔흡수지수,진일보건립해지수여토양함수량지간적선성의합관계래계산토양함수량。실험결과표명,여전통이용단일토양수분광보흡수특정삼수급기변형적방법상비,기우NSSAI구건적토양함수량반연모형의합정도교고(상관계수위0.93),재토양함수량교저화교고적정황하도능유효배제토양류형차이조성적영향,제고료라토토양함수량적반연정도。
Soil is the loose solum of land surface that can support plants .It consists of minerals ,organics ,atmosphere ,mois‐ture ,microbes ,et al .Among its complex compositions ,soil moisture varies greatly .Therefore ,the fast and accurate inversion of soil moisture by using remote sensing is very crucial .In order to reduce the influence of soil type on the retrieval of soil mois‐ture ,this paper proposed a normalized spectral slope and absorption index named NSSAI to estimate soil moisture .The modeling of the new index contains several key steps :Firstly ,soil samples with different moisture level were artificially prepared ,and soil reflectance spectra was consequently measured using spectroradiometer produced by ASD Company .Secondly ,the moisture ab‐sorption spectral feature located at shortwave wavelengths and the spectral slope of visible wavelengths were calculated after ana‐lyzing the regular spectral feature change patterns of different soil at different moisture conditions .Then advantages of the two features at reducing soil types’ effects was synthesized to build the NSSAI .Thirdly ,a linear relationship between NSSAI and soil moisture was established .The result showed that NSSAI worked better (correlation coefficient is 0 .93) than most of other traditional methods in soil moisture extraction .It can weaken the influences caused by soil types at different moisture levels and improve the bare soil moisture inversion accuracy .