# Characterization and Degradation of Masonry Mortar in Historic Brick Structures

Authors: Denis A. Brosnan
Journal: Journal of Structures
 (2014)

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## Abstract

This study characterized mortars from a masonry fortification in Charleston, South Carolina (USA), harbor where construction was during the period 1839–1860. This location for analysis was interesting because of the sea water impingement on the structure. The study was included as part of an overall structural assessment with restoration as an objective. The mortars were found to be cement, lime, and sand mixtures in proportions similar to ones expected from the historic literature, that is, one part binder to two parts of sand. The binder was found to be American natural cement, a substance analogous to the European Roman cement. The results suggest that the thermal history of the cement during manufacturing affected setting rate explaining why the cements were considered as variable during the mid-to-late 1800s. Fine pores were found in mortars exposed to sea water resulting from corrosion. Contemporary natural cement was shown to release calcium in aqueous solution. While this release of calcium is necessary for setting in natural and Portland cements, excessive calcium solution, as exacerbated by sea water contact and repointing with Portland cement mortars, was shown to result in brick scaling or decay through cryptoflorescence.


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## Body

## 1. Introduction

Assessments of historic masonry structures include precise documentation of dimensions and elevations, analysis of structural stability, and characterization of materials. The characterization is a prerequisite to restoration and repair to insure that compatible materials are used and to protect the historic character of the structure.Masonry mortars throughout history have been composed of a binder material, aggregates, and additions, the latter of which alter the properties of the mortar during application or enhance properties in the hardened condition. The binders developed through history include natural pozzolanic materials (as used by Greek and Roman societies), lime and hydraulic lime, Roman cements (called natural cement when manufactured in the USA), and Portland cement. The historical development of binders is presented in detail by Blezard [1], von Landsberg [2], Eckel [3], and Cummings [4]. Elsen [5] provides comprehensive references on binders. Weber et al. [6] describe Roman cements in Europe with characterization of mortars by chemical analysis and petrography. Callebaut et al. [7] used advanced analytical techniques in mortar characterizations.Aggregates for masonry mortars are generally described as “fine” to distinguish the larger aggregate particles and stones used in concrete. The fine aggregates include crushed rock and natural sands with national specifications published in modern times for aggregate gradation [5]. Other substances found in historic mortars include ashes, brick fragments or other ceramics particles, and natural fibers.Until the advent of specifications on mortar materials or properties of hardened mortar, masons mixed fine materials or binders with aggregates in volumetric proportions to obtain acceptable consistencies of fabrication of masonry structures. In contemporary language, these proportions along with water content provided consistency for troweling.The focus of this paper is on the application of advanced analytical techniques to supplement traditional analyses in characterizing masonry mortars in a selected historic structure, Fort Sumter National Monument located in Charleston, South Carolina (USA), harbor. A second purpose is determining if microscopic evidence exists for physical and chemical alteration of the mortars through corrosion and/or mineral alteration.Fort Sumter is a “Third System” USA fortification built on a sand bar in Charleston harbor with construction starting in 1829. The Fort’s construction began with careful placement of large granite blocks forming a peripheral foundation on the sand bar. After infill of the area encircled by the granite blocks with shells and sand, the brick wall construction began in 1841 using the materials and design principles dictated by General Joseph Gilbert Totten, Chief Engineer of the United States Army [8, 9]. As a young man, Totten studied use of Roman cements in Europe, and he subsequently specified use of the American analog to Roman cement, both known as “natural cement” and “Rosendale cement” in the USA.General Totten’s representatives typically specified Lawrence’s Rosendale Cement for bedding mortar. Totten’s mortar recipes were typically one part of cement to two parts of sand by volume. Acknowledging that the cement was a costly component when delivered at distant sites from New York, Totten states “It appears that when cement mortars are not required to be the strongest that can be made—a little lime may be added without great loss of tenacity, and, of course, with a saving of expense.” Totten allowed the use of a cement-lime-sand mortar of respective volumetric proportions 2 : 1 : 6.


## 2. Materials and Methods

Mortar specimens were obtained by removing bricks from the outermost wythe of bricks, that is, facing bricks, from the structure so as to obtain bedding mortar materials. All mortar materials were selected from the Eastern “Gorge Wall,” of the Fort that was rebuilt in the 1870s after substantial damage due to bombardment during the American Civil War. Care was taken to exclude any Portland cement pointing mortars applied to some sections of the exterior walls in the 1960s. For analysis purposes, a specimen of Rosendale cement was obtained from the current manufacturer, Edison Coatings, with that analysis being reported in Table1.Table 1
Chemical analysis of Rosendale cement.
Species
Historic reference 1 [10]
Historic reference 2 [11]
Modern Rosendale [12]
Contemporary Rosendale
Insoluble residue, contemporary Rosendale
CaO
27.8
33–60
35.3
46.3
1.1
MgO
12–21
19.2
22.8
0.3
Al2O3
5.5
5.5–10
5.5
4.3
8.3
SiO2
27.8
27–33
34.2
23.0
84.0
Fe2O3
4.3
2.6
1.8
1.5
TiO2
0.3
0.1
0.2
Na2O
0.5
0
1.6
K2O
2.2
1.8
2.9
Sum of constituents
99.8
100.1
99.9
Cementation index (CI)
1.66
0.90The techniques used in this mortar analysis are well known and conform to the literature citations provided. As cited earlier, Elsen published a review paper on the microscopy of historic mortars [5]. Krotzer and Walsh describe acid digestion techniques, instrumental analysis, and imaging techniques using polarized light microscopy [13]. The acid digestion techniques are described in standard methods [14]. Chiari et al. have used thermal analysis, a technique identifying weight changes and heat flow within materials during heating, to analyze historic mortars [15]. Brosnan et al. used combined techniques including chemical and mineralogical analysis, petrography, and thermal analysis to arrive at mortar compositions [16].


## 3. Results and Discussion

### 3.1. Cement Characterization

Cementitious materials are typically characterized by their chemical analysis or “assay” using constituents identified as metal oxide species per the convention employed by cement chemists. The analyses of Rosendale natural cement are shown in Table1. It is clear that oxides of calcium, magnesium, aluminum, silicon, and iron are the major constituents of the cement. Walsh and Uracius point out that the Rosendale cement is manufactured by burning/heating of argillaceous (clay containing) limestone [17].Natural cement was burned or “calcined” in periodic and continuous kilns so that it would “set,” that is, exhibit hydraulic activity, when ground and mixed with water. Mineral identification techniques including X-ray diffraction show that contemporary Rosendale cement contains major constituent minerals of anorthite—a calcium aluminosilicate (38.2%), quartz (28.7%), and microcline—a potassium aluminosilicate (12.6%). The familiar compounds in Portland cement are also present including alite—tricalcium silicate (6.4%) and belite—dicalcium silicate (4.0%). The content of amorphous phase and unidentified phases was 10.1%.These constituent minerals imply that a “set condition” (hardening) is attained after mixing cement with water through early carbonation of some compounds plus formation of calcium silicate phases. The cements can be compared on the basis of a cementation index (CI), the latter as delineated by Boynton [18], as follows:
(1)
CI
=
(
2.8
×
%
Si
O
2
+
1.1
×
%
Al
2
O
3
+
0.7
×
%
Fe
2
O
3
)
(
%
CaO
+
1.4
×
%
MgO
)
.The cementation index (CI) for modern Rosendale (Table1) of 1.66 is similar to the value of 1.65 reported by Weber for Roman cement. The variation in cementation index is apparently a characteristic of American natural cement. While results in historic references may be due to older analytical procedures, it is known that the American natural cements were highly variable in setting characteristics, and this fact has been attributed to their eventual demise.The thermal analysis of ground natural cement is shown in Figure1. This figure contains several results on the same graph making a careful inspection necessary.Figure 1
Thermal analysis of contemporary Rosendale cement. (TG: thermogravimetric trace, DSC: differential scanning calorimeter trace, water: water evolution trace, and CO2: carbon dioxide evolution trace).The thermal analysis provides the following important information:(1)
low temperature cement dehydration occurs below 500°C implying that the as-ground cement exhibits a content of phases normally expected in set cement after use; that is, there has been some formation of compounds during the cement in manufacture (as in grinding) and during storage prior to use. These phases may include carbonates and sulfates of the cement constituents;
(2)
the cement exhibits an endothermic/heat absorbing reaction at 575°C reflecting the presence of quartz “sand” in the cement rock (see also the insoluble residue analysis in Table1);
(3)
the cement exhibits a major decomposition of calcium carbonate at 722°C verifying that the cement was burned to an intermediate temperature between the decomposition temperature of magnesium carbonate, a constituent of dolomitic limestone in cement rock, and that of calcium carbonate also present in the cement rock.The fact that there is partial decomposition of the cement rock in manufacturing American natural cement strongly suggests that the setting characteristics of the cement are influenced by its thermal history. This is another reason for the consideration of historic natural cement as a variable product.The natural cement was additionally characterized by its release of soluble materials when placed in water suspension at room temperature (typically for 20 hours). The cement released about 15,000 parts per million (ppm) or 1.5% (by unit weight of cement) of calcium ions when 100 grams of cement was placed in 100 mL of deionized water at 20°C for 24 hours. The solution of potassium was particularly significant at 1357 ppm reflecting the argillaceous nature of the limestone. Another notable release of soluble material was sulfate at about 5000 ppm, and the decomposition of sulfates may explain the weight loss in the cement below 500°C (Figure1). The release of soluble metals such as calcium and potassium provides credence to the idea that the initial set/hardening of the cement, in part, is due to atmospheric carbonation processes and the formation of sulfates.


### 3.2. Mortar Characterization

Mortar analysis included determination of physical properties, chemical and mineralogical analysis, and microscopic examinations. Five mortar specimens were examined with three of the specimens obtained from positions above the mean high tide level and two from below ground or mean high tide level. The physical properties of the mortars are shown in Table2. All measurements were made using mercury intrusion porosimetry (MIP) because of the small size of the specimens. In MIP, mercury is forced into the pores of the specimen under pressure allowing for a calculation of the amount of porosity (apparent porosity) and for a calculation of the pore sizes present in the specimen.Table 2
Physical properties of mortar specimens (total mortar of binder and aggregate).
Specimen
Number 5 bedding mortar above sea level
Number  6 pointing mortar above sea level
Number 11 bedding mortar above sea level
Number 3  bedding mortar below sea level
Number 15  building, below infill soil level
Bulk density, Mg/m3
1.32
1.23
1.62
1.73
1.81
Apparent porosity, %
44.1
43.1
31.6
24.3
22.7
Percentage of porosity <1 micron in diameter
29.4
6.5
23.5
74.7
83.1The differences in density and apparent porosity of mortar likely reflect the local construction practices of the time. Lower bulk density and higher porosity usually reflect high water content in the mortar. The differences in density and porosity may reflect the rapid reconstruction of the Fort during an era of increased international tensions.It is interesting that the submerged mortars, constantly exposed to sea or ground salts, exhibit near normal porosity values, but they exhibit a significantly larger fraction of “fine” pores, that is, those less than one micron in diameter. Mortars above mean high tide level exhibit near normal porosities with no elevation in fraction of fine pores. The data suggests that salt water corrosion results in very high fractions of fine pores in fully or frequently submerged specimens.The chemical analyses by XRF and other data for the mortar specimens are shown in Table3 with one specimen analyzed per position on the Fort. For specimens not exposed to sea water, the magnesium oxide (MgO) content is a first suggestion that the mortars contained natural cement. Two of the mortars (numbers 3 and 5) exhibited very low calcium oxide (CaO) suggesting extreme solution of calcium from the mortar in sea water.Table 3
Chemical analyses and other data for Fort Sumter mortars (total mortar of binder and aggregate).
Specimen
Number 5  bedding mortar above sea level
Number  6  pointing mortar above sea sevel
Number 11  bedding mortar above sea level
Number  3  bedding mortar below sea level
Number 15  building, below infill soil level
CaO
0.73
54.57
12.30
0.74
26.79
MgO
9.20
15.53
5.05
0.72
11.59
Al2O3
1.21
2.84
0.96
1.75
2.00
SiO2 (Total)
82.63
22.11
80.28
88.33
57.73
Fe2O3
4.31
1.94
1.76
5.11
1.83
TiO2
1.25
0.15
<0.02
1.67
0.06
Na2O
<0.50
1.02
<0.50
<0.50
<0.50
K2O
0.70
1.83
0.14
1.68
<0.05
Sum of constituents
100.03
99.99
100.49
100.00
100.00
Insoluble residue, %
60.74
16.20
76.48
65.21
48.15
XRD mineralogy
Calcite, quartz, sodalite
Calcite, quartz
Calcite, quartz, sylvite
Calcite, quartz, iowaite, bassanite, brucite
Calcite, quartz, epidote
Soluble sodium or Na (ppm of solids)
839
2092
149
2066
851
Soluble calcium or Ca (ppm of solids)
3752
513
918
1807
3184
Soluble chloride or Cl (ppm of solids)
1232
2706
148
5801
7406
Soluble sulfate or SO4 (ppm of solids)
7218
1555
509
824
350
Rough mix proportions by volumecement : lime : sand
1 : 2 : 4
1 :2
1
2 : 1
4
1 : 4 : 9
ND
1 : 3.5 : 3All of the mortars exhibited water soluble species at room temperature. The mortars with low residual CaO content (numbers 3 and 5) exhibit high soluble sodium content (mortar 15 was exposed to ground salts, and the solution was exacerbated by salt water infiltration). Most mortars exhibited new mineral salts formed during service by salt water exposure (sodalite, sylvite, iowaite, bassanite, and epidote). Lubelli et al. [19] link chloride and sulfate in salt water to the solution of calcium from the mortars. This provides a likely reason for reduced CaO in some of the mortars at Fort Sumter.Petrographic analysis using polarized light microscopy confirmed the presence of Rosendale cement in the historic mortars. A typical photomicrograph is shown in Figure2 where a Rosendale cement relic (indicated as CR) is shown in the field with a lime relic (LR) and porosity (P) in a carbonate matrix. Scanning electron microscopy with energy dispersive X-ray analysis confirmed the phase identifications.Figure 2
Typical mortar photomicrograph (ca. 150x).All mortars contained silica sand typically exhibiting greater than 96% SiO2 when examined using scanning electron microscopy. The variation in CaO content in Table 3, a consequence of leaching by sea water of the lime phase, results in an effect of the value of the total analysis for SiO2 in the mortars.The rough mix proportions were determined using the insoluble residue as the aggregate content of the mortar, and the lime content was calculated using thermogravimetric data for each mortar (weight loss at the calcium carbonate decomposition). The balance was considered as the cement content. The volumetric proportions were calculated from standard densities for constituents per ASTM C1324. The proportions of the mortars (Table3) at least are conceptually similar to the Totten formula of one part of fine material (cement and lime) to two parts of sand. All of the bedding mortars exhibit a greater volumetric proportion of sand to fines. The rough mix proportions (Table 3) do not match the Totten formula exactly, and this was likely a consequence of local construction practices. The pointing mortar contains less sand than the bedding mortars as expected.


### 3.3. Structural Observations

One very interesting finding was salt scaling on the exterior walls of the Fort where there had been pointing repairs with ordinary Portland cement mortar (Figure3). This is a classic case of “brick scaling” caused by excessive solution of calcium from the repair mortar in the presence of sea salts as explained by Lubelli et al. [19]. The results suggest that the Portland cement mortar was a source of sufficient soluble calcium to cause the damage. Similar scaling failures are not seen on areas of the Fort that have not experienced repointing with Portland cement mortar.Figure 3
Salt scaling on the lower Fort walls pointed with Portland cement mortar.Such scaling is technically known as cryptoflorescence, and the scaling is due to subsurface expansions within the bricks via salt crystallization. Thus, cryptoflorescence is a damaging mechanism to the historic materials, while surface discolorations known as efflorescence are a nondamaging cosmetic defect in masonry.A cryptoflorescence failure on the Fort is shown together with scanning electron microscope photomicrographs in Figure4. On this face of the Fort, the Portland cement pointing mortar used in modern repairs has completely worn away revealing the “pink” colored Rosendale cement-based bedding mortar. The effect of the calcium solution from repair mortar and infiltration into the bricks with moisture is evident in the “cupped shape” of the residual brick. The scanning electron microscope investigation identified the mineral phase ettringite near the periphery of the brick. It is well known that the formation on ettringite results in expansive forces. This expansion resulted in damage to the historic bricks as shown in the photograph.Figure 4
Cryptoflorescence failures on Fort Sumter: macroscopic and microscopic (SEM) results.


## 3.1. Cement Characterization

Cementitious materials are typically characterized by their chemical analysis or “assay” using constituents identified as metal oxide species per the convention employed by cement chemists. The analyses of Rosendale natural cement are shown in Table1. It is clear that oxides of calcium, magnesium, aluminum, silicon, and iron are the major constituents of the cement. Walsh and Uracius point out that the Rosendale cement is manufactured by burning/heating of argillaceous (clay containing) limestone [17].Natural cement was burned or “calcined” in periodic and continuous kilns so that it would “set,” that is, exhibit hydraulic activity, when ground and mixed with water. Mineral identification techniques including X-ray diffraction show that contemporary Rosendale cement contains major constituent minerals of anorthite—a calcium aluminosilicate (38.2%), quartz (28.7%), and microcline—a potassium aluminosilicate (12.6%). The familiar compounds in Portland cement are also present including alite—tricalcium silicate (6.4%) and belite—dicalcium silicate (4.0%). The content of amorphous phase and unidentified phases was 10.1%.These constituent minerals imply that a “set condition” (hardening) is attained after mixing cement with water through early carbonation of some compounds plus formation of calcium silicate phases. The cements can be compared on the basis of a cementation index (CI), the latter as delineated by Boynton [18], as follows:
(1)
CI
=
(
2.8
×
%
Si
O
2
+
1.1
×
%
Al
2
O
3
+
0.7
×
%
Fe
2
O
3
)
(
%
CaO
+
1.4
×
%
MgO
)
.The cementation index (CI) for modern Rosendale (Table1) of 1.66 is similar to the value of 1.65 reported by Weber for Roman cement. The variation in cementation index is apparently a characteristic of American natural cement. While results in historic references may be due to older analytical procedures, it is known that the American natural cements were highly variable in setting characteristics, and this fact has been attributed to their eventual demise.The thermal analysis of ground natural cement is shown in Figure1. This figure contains several results on the same graph making a careful inspection necessary.Figure 1
Thermal analysis of contemporary Rosendale cement. (TG: thermogravimetric trace, DSC: differential scanning calorimeter trace, water: water evolution trace, and CO2: carbon dioxide evolution trace).The thermal analysis provides the following important information:(1)
low temperature cement dehydration occurs below 500°C implying that the as-ground cement exhibits a content of phases normally expected in set cement after use; that is, there has been some formation of compounds during the cement in manufacture (as in grinding) and during storage prior to use. These phases may include carbonates and sulfates of the cement constituents;
(2)
the cement exhibits an endothermic/heat absorbing reaction at 575°C reflecting the presence of quartz “sand” in the cement rock (see also the insoluble residue analysis in Table1);
(3)
the cement exhibits a major decomposition of calcium carbonate at 722°C verifying that the cement was burned to an intermediate temperature between the decomposition temperature of magnesium carbonate, a constituent of dolomitic limestone in cement rock, and that of calcium carbonate also present in the cement rock.The fact that there is partial decomposition of the cement rock in manufacturing American natural cement strongly suggests that the setting characteristics of the cement are influenced by its thermal history. This is another reason for the consideration of historic natural cement as a variable product.The natural cement was additionally characterized by its release of soluble materials when placed in water suspension at room temperature (typically for 20 hours). The cement released about 15,000 parts per million (ppm) or 1.5% (by unit weight of cement) of calcium ions when 100 grams of cement was placed in 100 mL of deionized water at 20°C for 24 hours. The solution of potassium was particularly significant at 1357 ppm reflecting the argillaceous nature of the limestone. Another notable release of soluble material was sulfate at about 5000 ppm, and the decomposition of sulfates may explain the weight loss in the cement below 500°C (Figure1). The release of soluble metals such as calcium and potassium provides credence to the idea that the initial set/hardening of the cement, in part, is due to atmospheric carbonation processes and the formation of sulfates.


## 3.2. Mortar Characterization

Mortar analysis included determination of physical properties, chemical and mineralogical analysis, and microscopic examinations. Five mortar specimens were examined with three of the specimens obtained from positions above the mean high tide level and two from below ground or mean high tide level. The physical properties of the mortars are shown in Table2. All measurements were made using mercury intrusion porosimetry (MIP) because of the small size of the specimens. In MIP, mercury is forced into the pores of the specimen under pressure allowing for a calculation of the amount of porosity (apparent porosity) and for a calculation of the pore sizes present in the specimen.Table 2
Physical properties of mortar specimens (total mortar of binder and aggregate).
Specimen
Number 5 bedding mortar above sea level
Number  6 pointing mortar above sea level
Number 11 bedding mortar above sea level
Number 3  bedding mortar below sea level
Number 15  building, below infill soil level
Bulk density, Mg/m3
1.32
1.23
1.62
1.73
1.81
Apparent porosity, %
44.1
43.1
31.6
24.3
22.7
Percentage of porosity <1 micron in diameter
29.4
6.5
23.5
74.7
83.1The differences in density and apparent porosity of mortar likely reflect the local construction practices of the time. Lower bulk density and higher porosity usually reflect high water content in the mortar. The differences in density and porosity may reflect the rapid reconstruction of the Fort during an era of increased international tensions.It is interesting that the submerged mortars, constantly exposed to sea or ground salts, exhibit near normal porosity values, but they exhibit a significantly larger fraction of “fine” pores, that is, those less than one micron in diameter. Mortars above mean high tide level exhibit near normal porosities with no elevation in fraction of fine pores. The data suggests that salt water corrosion results in very high fractions of fine pores in fully or frequently submerged specimens.The chemical analyses by XRF and other data for the mortar specimens are shown in Table3 with one specimen analyzed per position on the Fort. For specimens not exposed to sea water, the magnesium oxide (MgO) content is a first suggestion that the mortars contained natural cement. Two of the mortars (numbers 3 and 5) exhibited very low calcium oxide (CaO) suggesting extreme solution of calcium from the mortar in sea water.Table 3
Chemical analyses and other data for Fort Sumter mortars (total mortar of binder and aggregate).
Specimen
Number 5  bedding mortar above sea level
Number  6  pointing mortar above sea sevel
Number 11  bedding mortar above sea level
Number  3  bedding mortar below sea level
Number 15  building, below infill soil level
CaO
0.73
54.57
12.30
0.74
26.79
MgO
9.20
15.53
5.05
0.72
11.59
Al2O3
1.21
2.84
0.96
1.75
2.00
SiO2 (Total)
82.63
22.11
80.28
88.33
57.73
Fe2O3
4.31
1.94
1.76
5.11
1.83
TiO2
1.25
0.15
<0.02
1.67
0.06
Na2O
<0.50
1.02
<0.50
<0.50
<0.50
K2O
0.70
1.83
0.14
1.68
<0.05
Sum of constituents
100.03
99.99
100.49
100.00
100.00
Insoluble residue, %
60.74
16.20
76.48
65.21
48.15
XRD mineralogy
Calcite, quartz, sodalite
Calcite, quartz
Calcite, quartz, sylvite
Calcite, quartz, iowaite, bassanite, brucite
Calcite, quartz, epidote
Soluble sodium or Na (ppm of solids)
839
2092
149
2066
851
Soluble calcium or Ca (ppm of solids)
3752
513
918
1807
3184
Soluble chloride or Cl (ppm of solids)
1232
2706
148
5801
7406
Soluble sulfate or SO4 (ppm of solids)
7218
1555
509
824
350
Rough mix proportions by volumecement : lime : sand
1 : 2 : 4
1 :2
1
2 : 1
4
1 : 4 : 9
ND
1 : 3.5 : 3All of the mortars exhibited water soluble species at room temperature. The mortars with low residual CaO content (numbers 3 and 5) exhibit high soluble sodium content (mortar 15 was exposed to ground salts, and the solution was exacerbated by salt water infiltration). Most mortars exhibited new mineral salts formed during service by salt water exposure (sodalite, sylvite, iowaite, bassanite, and epidote). Lubelli et al. [19] link chloride and sulfate in salt water to the solution of calcium from the mortars. This provides a likely reason for reduced CaO in some of the mortars at Fort Sumter.Petrographic analysis using polarized light microscopy confirmed the presence of Rosendale cement in the historic mortars. A typical photomicrograph is shown in Figure2 where a Rosendale cement relic (indicated as CR) is shown in the field with a lime relic (LR) and porosity (P) in a carbonate matrix. Scanning electron microscopy with energy dispersive X-ray analysis confirmed the phase identifications.Figure 2
Typical mortar photomicrograph (ca. 150x).All mortars contained silica sand typically exhibiting greater than 96% SiO2 when examined using scanning electron microscopy. The variation in CaO content in Table 3, a consequence of leaching by sea water of the lime phase, results in an effect of the value of the total analysis for SiO2 in the mortars.The rough mix proportions were determined using the insoluble residue as the aggregate content of the mortar, and the lime content was calculated using thermogravimetric data for each mortar (weight loss at the calcium carbonate decomposition). The balance was considered as the cement content. The volumetric proportions were calculated from standard densities for constituents per ASTM C1324. The proportions of the mortars (Table3) at least are conceptually similar to the Totten formula of one part of fine material (cement and lime) to two parts of sand. All of the bedding mortars exhibit a greater volumetric proportion of sand to fines. The rough mix proportions (Table 3) do not match the Totten formula exactly, and this was likely a consequence of local construction practices. The pointing mortar contains less sand than the bedding mortars as expected.


## 3.3. Structural Observations

One very interesting finding was salt scaling on the exterior walls of the Fort where there had been pointing repairs with ordinary Portland cement mortar (Figure3). This is a classic case of “brick scaling” caused by excessive solution of calcium from the repair mortar in the presence of sea salts as explained by Lubelli et al. [19]. The results suggest that the Portland cement mortar was a source of sufficient soluble calcium to cause the damage. Similar scaling failures are not seen on areas of the Fort that have not experienced repointing with Portland cement mortar.Figure 3
Salt scaling on the lower Fort walls pointed with Portland cement mortar.Such scaling is technically known as cryptoflorescence, and the scaling is due to subsurface expansions within the bricks via salt crystallization. Thus, cryptoflorescence is a damaging mechanism to the historic materials, while surface discolorations known as efflorescence are a nondamaging cosmetic defect in masonry.A cryptoflorescence failure on the Fort is shown together with scanning electron microscope photomicrographs in Figure4. On this face of the Fort, the Portland cement pointing mortar used in modern repairs has completely worn away revealing the “pink” colored Rosendale cement-based bedding mortar. The effect of the calcium solution from repair mortar and infiltration into the bricks with moisture is evident in the “cupped shape” of the residual brick. The scanning electron microscope investigation identified the mineral phase ettringite near the periphery of the brick. It is well known that the formation on ettringite results in expansive forces. This expansion resulted in damage to the historic bricks as shown in the photograph.Figure 4
Cryptoflorescence failures on Fort Sumter: macroscopic and microscopic (SEM) results.


## 4. Conclusions

Use of natural or Rosendale cement was confirmed as a constituent of the mortars by a combination of traditional and advanced analytical techniques. The advanced techniques provide rapid and complimentary results so that the mortar constituents are identified for restoration purposes. Further, mortar batch compositions were similar to those expected from the historical record.The sea salt exposure produced characteristic fine pores within the mortar reflecting calcium removal via corrosion. Calcium removal also resulted in salt scaling or cryptoflorescence on the masonry walls as seen on brick surfaces. It is important that structural analysts recognize salt scaling on bricks and its possible causation in excessive calcium solution from masonry mortar.



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*Source: 859879-2014-04-27.xml*