CAJ | 학술논문

干旱半干旱地区湿地土壤中的有机碳是影响土壤质量，制约植物生长的重要因素之一，其含量的变化会影响生态系统的安全和稳定。为快速估测湿地土壤有机碳含量，在新疆艾比湖湿地保护区采集140个荒漠土壤样品，利用土壤可见/近红外光谱数据以及化学分析获取的土壤有机碳数据，在对土壤原始光谱反射率进行卷积平滑的基础上，获取了一阶微分、倒数对数一阶微分2种光谱预处理指标，采用蚁群-区间偏最小二乘法、基于支持向量机的回归特征消去法，选择土壤有机碳含量近红外光谱特征波长，在此基础上构建土壤有机碳含量偏最小二乘回归、支持向量回归模型。结果表明：1）利用原始一阶微分建立的模型，预测能力优于倒数对数一阶微分建立的模型。2）4种建模结果比较显示，利用原始一阶微分经基于支持向量机的回归特征消去法进行特征变量选择后建立的土壤有机碳含量模型，预测精度最高。训练集的相关系数以及均方根误差分别为0.9687、0.158%；测试集的相关系数和均方根误差分别为0.9091以及0.268%。因此，经过卷积平滑以及一阶微分预处理、并利用基于支持向量机的回归特征消去法建立的模型具有较高的预测精度和较好的稳健性，可以作为有效手段估算荒漠湿地土壤有机碳含量。
간한반간한지구습지토양중적유궤탄시영향토양질량，제약식물생장적중요인소지일，기함량적변화회영향생태계통적안전화은정。위쾌속고측습지토양유궤탄함량，재신강애비호습지보호구채집140개황막토양양품，이용토양가견/근홍외광보수거이급화학분석획취적토양유궤탄수거，재대토양원시광보반사솔진행권적평활적기출상，획취료일계미분、도수대수일계미분2충광보예처리지표，채용의군-구간편최소이승법、기우지지향량궤적회귀특정소거법，선택토양유궤탄함량근홍외광보특정파장，재차기출상구건토양유궤탄함량편최소이승회귀、지지향량회귀모형。결과표명：1）이용원시일계미분건립적모형，예측능력우우도수대수일계미분건립적모형。2）4충건모결과비교현시，이용원시일계미분경기우지지향량궤적회귀특정소거법진행특정변량선택후건립적토양유궤탄함량모형，예측정도최고。훈련집적상관계수이급균방근오차분별위0.9687、0.158%；측시집적상관계수화균방근오차분별위0.9091이급0.268%。인차，경과권적평활이급일계미분예처리、병이용기우지지향량궤적회귀특정소거법건립적모형구유교고적예측정도화교호적은건성，가이작위유효수단고산황막습지토양유궤탄함량。
Soil organic carbon (SOC) is a critical soil property that has profound impact on soil quality and plant growth. It is involved in soil structural formation and atmospheric carbon sequestration. This is especially true in the arid and semi-arid regions. Accurately detecting SOC is an important issue. Traditionally, SOC is limited to laboratory determination using the techniques such as wet or dry combustion, ion sensing electrodes, loss on ignition, or via chemical assays. Yet those traditional approaches often involve expensive testing materials, time-consuming sample preparation and production of excessive environmental pollutants. An approach which can quantify SOC content with time and cost savings is needed. With 140 soil samples acquired from the Ebinur Lake wetland protection area in Xinjiang, China, this research attempts to apply 2 algorithms in hyperspectral data mining, namely, the ant colony optimization – interval partial least squares (ACO-iPLS) and recursive feature elimination – support vector machine (SVM-RFE) to improve the estimation accuracy of SOC content using the visible and near-infrared (VIS/NIR) spectroscopy of soils (350-2500 nm) in laboratory. After convolution smoothing (S-G), 2 common spectra pre-processing methods, namely, first order differential and first order differential of the logarithm of inverse, are applied in the hyperspectral data to extract the feature wavelengths. Results indicate that the feature wavelengths pertaining to SOC mainly are located within 1786-1929 nm with ACO-iPLS and 745-910, 1677, 1755, and 1911-2254 nm with SVM-RFE. With the extracted feature wavelengths, the ensuing models with the same 2 approaches are established with the half of the samples (70 soil samples) as training set and the other half (70 soil samples) as testing set. The results show that the spectra processed with the combination of the S-G and first order with reflectance perform much better than the logarithm of first order differential of the logarithm of inverse after the S-G. Compared to the linear model used commonly, i.e. ACO-iPLS, the nonlinear model SVM-RFE pre-processed with first order differential with reflectance produces the higher estimation accuracy. The root mean square error of cross validation (RMSECV) and the root mean square error of prediction (RMSEP) for the SVM-RFE approach are respectively 0.158% and 0.268% in the training and testing set. The correlation coefficient of cross validation (Rcv) and the correlation coefficient of prediction (Rp) are 0.9687 and 0.9091, respectively. The relative prediction deviation (RPD) of testing set is 2.41. The RMSECV and RMSEP for the ACO-iPLS approach are respectively 0.329% and 0.396% in the training and testing set. The Rcv and Rp are 0.8647 and 0.8297, respectively. The RPD of the testing set is 1.63. The SVM-RFE approach pre-processed with first order differential of the logarithm of inverse produces the higher estimation accuracy than the ACO-iPLS. The RMSECV and RMSEP for the SVM-RFE approach are 0.033% and 0.448%, respectively. The Rcv and Rp are 0.9989 and 0.8111, respectively. The RPD of testing set is 1.44. The RMSECV and RMSEP for the ACO-iPLS approach are 0.496% and 0.586%, respectively. The Rcv and Rp are 0.7293 and 0.586, respectively. The RPD of the testing set is 1.10. Over all, the good performance of the SVM model can be ascribed to its good capability of dealing with non-linear and hierarchical relationship between SOC and feature wavelengths. The results are fairly satisfactory. This practice provides an efficient, low-cost, potentially highly accurate approach to estimate SOC content and hence support better management and protection strategies for desert wetland ecosystems. The next step is to attempt to apply VIS/NIR spectroscopy technique in the field for further research.