Sunil Kr. Jha and Zulfiqar Ahmad
The soil is the lively part of the terrestrial environment that supports all forms of life.Soil condition is the result of continuous conservation and degradation processes and represents its continued capacity to function as vital living ecosystems [Carter, Gregorich and Anderson et al. (1997); Doran, Jones and Arshad et al. (1999); Doran and Zeiss(2000); Ghosh, Palsaniya and Kumar (2017)]. A unique balance of chemical, physical and biological (including microbial) components contribute to maintaining soil strength[Or, Smets and Wraith et al. (2007); Schoenholtz, Van Miegroet and Burger (2000); Doran(2002); Nielsen, Winding and Binnerup et al. (2002)]. Consequently, the assessment of soil strength necessitates the estimations of its components. Microorganisms possess the ability to contribute an integrated measure of soil condition that cannot be obtained with physical/chemical measures [Nielsen, Winding and Binnerup et al. (2002); Winding, Hund-Rinke and Rutgers (2005); Fine, Van Es and Schindelbeck (2017)]. Microorganisms respond quickly to changes, hence they rapidly adapt to environmental conditions. The microorganisms that are best adapted will be the ones that flourish [Singh, Pandey and Singh (2011); Ali, Hayat and Begum et al. (2017)]. This adaptation potentially allows microbial analyses to be discriminating in soil fitness assessment, and changes in microbial populations and activities, therefore, function as an excellent indicator of change in soil condition [Schloter, Dilly and Munch (2003); Gil-Sotres, Trasar-Cepeda and Leiró s et al. (2005); Van Bruggen and Semenov (2000); Hermans, Buckley and Case et al. (2016)]. Microbial indicators of soil condition cover a diverse set of microbial capacities due to the multifunctional properties of microbial communities in the soil ecosystem that support to (i) control plant diseases as well as insect and weed pests; (ii)form beneficial symbiotic associations with plant roots (e.g. nitrogen-fixing bacteria and mycorrhizal fungi); (iii) recycle plant nutrients; (iv) improve soil structure with positive repercussions for its water- and nutrient-holding capacity; and (v) increase crop production [Ros, Goberna and Moreno et al. (2006); Alkorta, Aizpurua and Riga et al.(2003); Havlicek, (2012); Garbach, Milder and DeClerck et al. (2017); Tamez-Hidalgo,Christensen and Lever et al. (2016)]. One of the most important objectives in assessing the condition of a soil is the establishment of indicators for evaluating its current status[Doran, Jones and Arshad et al. (1999); Doran (2002); Schipper and Sparling (2000)].Microbial population and enzyme activity are significant soil microbial condition indicators. These factors can be modeled using statistical and artificial intelligence techniques with significantly less engineering effort [Barberá n, Bates and Casamayor et al. (2012); Hughes, Hellmann and Ricketts et al. (2001); Haider, Pakshirajan and Singh et al. (2008); Liang, Das and McClendon (2003); Tajik, Ayoubi and Nourbakhsh (2012);Kim, Yoo and Ki et al. (2011); Ebrahimi, Sinegani and Sarikhani et al. (2017); Ludwig,Vormstein and Niebuhr et al. (2017); Mukhlisin, El-Shafie and Taha (2012); Taghavifar and Mardani (2014)]; meanwhile, soil microbial, enzyme activity prediction by mathematical models is a tough task. In recent years, the trends towards modeling of machining processes using artificial intelligence methods have been increased due to their advanced computing capability. Researchers have used various intelligent techniques, including artificial neural network (ANN), fuzzy logic, neuro-fuzzy, adaptive neuro-fuzzy inference system (ANFIS) etc., for the prediction of machining parameters and to enhance manufacturing automation [Sen, Mandal and Mondal (2017); Yu, Yu and Wang et al. (2016); Hanafy, Zaini and Shoush et al. (2014)]. ANN and fuzzy logic are two important methods of artificial intelligence in modeling nonlinear problems. For example, ANN model has been implemented in the prediction of biosurfactant production under variable environmental conditions [Ahmad, Crowley and Marina et al.(2016)]. A neural network can learn from the data and feedback, however understanding the knowledge or the pattern is difficult. On the other hand, fuzzy logic models are easy to comprehend because they use linguistic terms in the form ofif-thenrules. A neural network with their learning capabilities can be also used to learn the fuzzy decision rules,to create a hybrid intelligent system. A powerful subtractive clustering (SC) and Wang and Mendel’s (WM) rule-based fuzzy inference systems (FIS) have been implemented in various application domains [Eftekhari and Katebi (2008); Lohani, Goel and Bhatia(2014); Wang (2003); Yang, Yuan and Yuan et al. (2010)]. Both methods use the advantages of fuzzy systems in a different way in efficient predicting and modeling.Though, we hardly noticed the implementation of FIS methods in soil microbial dynamics prediction in published literature. The FIS method in modeling and optimization problems is an effective way for the number of trials, and saving time and materials as well as offering a complete evaluation of the experimental process through creating a regression relation between dependent and independent variables. With this motivation, in the present research, evaluation and comparison of the prediction and simulation efficiency of SC-FIS and WM-FIS methods have been accomplished for estimation of soil microbial dynamics under fluctuating environmental situations.
Fuzzy logic is based on degrees of truth than completely true or false, which is similar to the functioning of the human brain. Both gather data about an incident, create a number of partial truths, and finally compose them into a higher truth. In data mapping, fuzzy logic assigns partial membership to each data point rather than the complete membership.After that, partial memberships are composed using certainif-thenrules to find out the complete membership [Klir and Yuan (1995)]. Fuzzy inference is the process of constructing the map from a given input to an output using the fuzzy logic approach.Mainly, clustering methods, including the c–means clustering, fuzzy c–means clustering,mountain clustering, and subtractive clustering are used for generating the fuzzy rules in inference system. In the present study, most widely used subtractive clustering method is used in the implementation of fuzzy inference system and their performance is compared with the general fuzzy inference system based on Wang and Mendel’s rule. A short description of both methods is as follows.
Wang and Mendel’s (WM) fuzzy rule based system (FRBS) is the simplest type of inference system. It is implemented in the present study by using thefrbspackage in R[Riza, Bergmeir and Herrera et al. (2015)]. For a particular data set,whererepresent the output of input pair, basic steps of method are as follows[Wang and Mendel (1982)]: (a) partitioning of input and output spaces into fuzzy regions by dividing the domain interval of each input and output variable intoregions,wheremay be different for each of the variables with either equal or unequal length,and assigning membership function to each partition; (b) generating fuzzy rules for the data pairs using the training data set after partitioning from the previous step by deciding the degrees of each input-output pairs to different regions, assigning pairs to a maximum degree and obtaining one if-then rule for one pair; (c) assigning a degree to each rule,this is done to avoid the inconsistent rules of similarifpart and differentthenpart for different data pairs; (d) creating a combined rule base, and (e) mapping based on a combined fuzzy rule. The details of the method can be seen in Ref. [Wang and Mendel(1982)].
The Subtractive clustering (SC) finds fuzzy clusters by assigning each data point a potentialfor the likelihood of it according to a Gaussianthe cluster radius. The Euclidean normsignifies the vector distance between data points. The data point with maximum potential is selected as the first cluster center and all the data points within distanceof cluster center are linked to the first cluster. The second cluster center is determined in a similar way after excluding the data points associated with the first cluster. The process is continued until all data points lie withinof a cluster center [Chiu (1994); Chiu (1997)].In this way, the subtractive clustering method produces a number of clusters in the data set for generating fuzzy rules in following steps: (a) degree of fulfillment ofithfuzzy rule fromithcluster center is calculated asfor eachjthinput toithfuzzy rule as;using the fuzzyrule. The details of fuzzy rule extraction are described in [Chiu(1994); Chiu (1997)]. The method is implemented using thefrbspackage in R [Riza,Bergmeir and Herrera et al. (2015)].
The rhizospheric soil was collected from the wheat field. For this purpose, wheat plants were uprooted at tillering stage and stored in polythene bags. The non-rhizospheric soil was removed by agitating the roots strongly and the soil strictly adhering to the roots was used for the desired soil sample. Seven different wheat rhizospheric samples were collected and pooled up to make a composite sample and designated wheat root rhizospheric samples (WRS). The measured input experimental parameters using the Taguchi design are summarized in Table 1. Measured values of the bacterial population,rock phosphate solubilization, and ACC deaminase activity is given in Table 2.
Table 1: Values of different input variables.
Table 2: Measured average value of rock phosphate solubilization, bacterial population,and ACC deaminase activity.
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3.2.1 Phosphate solubilization activity measurements
The phosphorus solubilizing activity of bacterial isolates present in soil sample was determined on the basis of the extent of solubilization of rock phosphate in NBRIP broth media [Nautiyal (1999)]. Briefly, 0.1 g rhizospheric soil sample was dissolved in 100 mL Tryptic soy broth in a conical flask and placed in shaking incubator at 100 rpm at 28oC.After 18 hrs incubation, the bacterial growth was observed by turbidity. For rock phosphate solubilization, 20 μL of prepared inoculums was added to 50 mL, modified NBRIP broth (Glucose 10g, Rock phosphate 5g, MgCl2.6H2O 5g, MgSO4.7H2O 0.25g,KCl 0.2g, (NH4)2SO40.1g/L). Respective control was run without inoculums from rhizospheric soil samples. After 72 hrs of incubation, in shaking incubator, broth inoculated media was filtered and available P contents were measured at 410 nm [Olsen and Sommers (1982)]. The experiment was performed in replicate.
3.2.2 Bacterial population measurement
Cultivable attached rhizospheric bacteria were counted by the spread plate method on Marine Agar (Difco 2216) sterilized by autoclaving (121°C, 1 atm for 20 min). Dilutions were performed in 34 g/L sterile sodium chloride solution. Plates were set up in duplicate for each dilution. Incubation times were, according to the experimental at 25°C.Bacterial concentrations were expressed as CFU per ml for cultivable bacteria [Leonard,Blancheton and Guiraud (2000)].
3.2.3 Quantification of ACC deaminase activity measurementACC deaminase activity was assayed according to the method described by Penrose and Glick [Penrose and Glick (2003)], which measures the amount of α-ketobutyrate produced after the enzyme ACC deaminase, cleaves ACC. The quantity of αketobutyrate (Sigma-Aldrich Co., U.S.A.) produced by this reaction was determined by comparing the absorbance of a sample to a standard curve of α-ketobutyrate ranging between 0.1-1.0 nmol at 540 nm. A stock solution of α-ketobutyrate was prepared in 0.1 M Tris-HCl (pH 8.5) and stored at 4oC. In order to measure the specific activity of the cultures, protein estimation was carried out according to the procedure detailed in[Lowly (1951)]. The data were subjected to analysis of variance using Statix software and means were compared by Duncan’s multiple range tests at 5% probability [Steel and Torrie (1980)].
The predicted values of phosphate solubilization (PS), bacterial population (BP), and ACC deaminase activity (ACCA) by WM-FIS and SC-FIS methods are exhibited in Figs.1-3 respectively. The accuracy of both FIS methods has been evaluated in terms of the Pearson correlation coefficient (ρ), root mean square error (RMSE), and coefficient of determination (R2) are computed according to Eq. 1-3 [Steel and Torrie (1980)],respectively and have been summarized in Table 3.
WM-FIS and SC-FIS methods have been implemented in the estimation of phosphate solubilization, bacterial population and ACC deaminase activity and their performance are compared in terms of the Pearson correlation coefficient, root mean square error and coefficient of determination. The Pearson correlation coefficient indicates the strength of the relationship between the actual values of phosphate solubilization, bacterial population and ACC deaminase activity and their estimated values by WM-FIS and SCFIS methods, but the coefficient of determination measures the definite strength.
Figure 1: Phosphate solubilization estimation results using WM-FIS and SC-FIS methods.
Figure 2: Bacterial population estimation results using WM-FIS and SC-FIS methods.
Figure 3: Bacterial population estimation results using WM-FIS and SC-FIS methods.
Table 3: Values of different input variables.
The correlation coefficient close to one indicates an approximately linear relationship between the actual and model predicted values of a dependent variable as well as better performance of model used for estimation. The RMSE is a significant measure to explain the precision of the model used for prediction, though; it is sensitive to large errors. The coefficient of determination is a significant measure to check the performance of models used in the estimation as it helps to understand the inconsistency of dependent variables.Fig. 1 presents the actual phosphate solubilization vs. WM-FIS and SC-FIS model predicted phosphate solubilization on a log scale. It is obvious that the SC-FIS model predicted values of phosphate solubilization are comparable to the experimental values of phosphate solubilization (except for measurement number 40). Though, the WM-FIS model predicted values of phosphate solubilization exhibit larger deviation to the experimental values. This fact is further confirmed by the minimum value ofand maximum values of the correlation coefficientand the coefficient of determination(Table 3) for the SC-FIS model than the WM-FIS model predicted values of phosphate solubilization. Also, SC-FIS model has a better estimation efficiency for the phosphate solubilization than bacterial population and ACC deaminase activity in terms of,and. The prediction results of the bacterial population using SC-FIS and WM-FIS methods have been shown in Fig. 2. Again, SC-FIS method exhibits better estimation efficiency than the WM-FIS method (except measurement number 2). This is also established with the lesser value ofand higher values of the correlation coefficientand the coefficient of determinationfor the SC-FIS model than the WM-FIS model in the prediction of bacterial population (Table 3). The ACC deaminase activity estimation results are shown in Fig. 3.In most of the measurements, the SC-FIS model estimated values of ACC deaminase activity are closer to their real measured values. This confirms the better performance of the SC-FIS model than the WM-FIS model. This fact is further approved in terms of afor the SC-FIS model than the WMFIS model (Table 3). During the analysis, it is observed that there is some combination of input variables that results in the SC-FIS and WM-FIS model predicted values of phosphate solubilization, bacterial population and ACC deaminase activity close to their actual values. Table 4 summarizes three best combinations of such variables. In case of phosphate solubilization, SC-FIS method for the combination of input parameters:,, andresults in almost 100% accuracy in prediction(actual value of phosphate solubilization 113.59 and SC-FIS method predicted value of phosphate solubilization 113.56). A similar situation is observed for two combinations of input parameters (, and,,) in the estimation of bacterial population using the SC-FIS method (Table 4). For ACC deaminase activity estimation using the SC-FIS method three combinations of input parameters(, and,,) results in almost 100% prediction accuracy. The best combinations of input parameters summarized in Table 4 can be used in searching the optimal environmental conditions that result in the best estimation of microbial dynamics. Fuzzy methods are accurate in the modeling of data while controlling the imprecision. Due to this reason, WM-FIS method has been implemented in several applications, like the prediction of dissolved oxygen in river water [Shaghaghian (2010)], operator performance using electroencephalographic (EEG) variables [Zhang, Xia and Garibaldi et al. (2017)], and energy forecasting [Jozi, Pinto and Pra? a et al. (2016)]. Also, the WM-FIS method has reliable prediction performance than ANN and support vector machine (SVM) methods in the latter application. Though, the application of WM-FIS method in microbial dynamics estimation is not noticed in published literature. Also, the performance of WM-FIS method has been enhanced in some recent studies, like using an evolutionary algorithm in controlling fuzzy sets [Kato, Morandin and Sgavioli et al. (2009)], and inducing cooperation for fuzzy rules [Casillas, Cordó n and Herrera (2000)], etc. Another option is to evaluate the performance of WM-FIS method with some other FIS method like SC-FIS which has better efficiency in several applications like road header performance prediction [Yazdani-Chamzini, Razani and Yakhchali et al. (2013)], fault detection [Chudasama, Shah and Shah (2016)], modeling demand response of smart grid[Pereira, Fagundes and Melicio et al. (2014)], and soil cation exchange capacity[Keshavarzi, Sarmadian and Rahmani et al. (2012)], etc. The better performance of the SC-FIS method is noticed than the WM-FIS method in the present analysis. Since the SC method recognizes similarities in the data set and creates an FIS to model the data behavior using a minimum number of efficient fuzzy rules. The prediction of ACC deaminase is significant as it is an important factor to promote the growth of a plant.
The study presents the estimation of microbial dynamics, including phosphate solubilization, bacterial population, and ACC-deaminase activity by using SC-FIS and WM-FIS methods and their performance is compared in terms of correlation coefficient,root mean square error and coefficient of determination. The temperature, pH, and incubation period show variation during the measurement and affects microbial dynamics, therefore used as input of SC-FIS and WM-FIS methods. The SC-FIS method has abetter estimation efficiency than the WM-FIS method of estimation of microbial dynamics. Also, the best estimation efficacy is observed for the phosphate solubilization by using the SC-FIS method. Estimation of ACC-deaminase activity by using WM-FIS method results in the least accuracy.
Acknowledgement:This work is supported by The Startup Foundation for Introducing Talent of NUIST. The authors acknowledge Dr. S.S. Murthy for his motivation and support and reviewers for their valuable comments and suggestions.
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Computer Modeling In Engineering&Sciences2017年4期