Normal myocardium has low to intermediate signal on T2W images, but increased regional water content, such as infarct related edema, causes an increase in the T2-relaxation time and T2W signal intensity [
15]. Hemorrhage and the breakdown of oxygenated hemoglobin also influence magnetic properties of the surrounding tissue. The effects of hemoglobin degradation have been extensively studied in patients with cerebral hemorrhage; they are complex and strongly dependent on the age of the hematoma and the integrity of the erythrocyte membrane [
8]. T2W signal is high in the very early, hyperacute phase, but then falls because of the paramagnetic effects of deoxyhemoglobin and intracellular methemoglobin [
8]. Especially in the core of the hematoma, where there is marked hypoxia, signal may remain very low for a prolonged period of time [
16]. Lotan et al. studied IMH in a canine myocardial infarction model using ex-vivo T2W [
9]. They found areas of low signal within the zone of increased signal that accurately matched the location of macroscopic hemorrhage in all animals but one (with a very small hemorrhage), and no hypointense T2W regions in the animals without hemorrhage. Hemorrhage size according to CMR correlated closely to size determined from tissue slices and according to labeled red blood cells. Basso et al. recently compared in vivo and ex-vivo CMR to histopathological findings in two patients that had died 12 and 24 days after percutaneous revascularization, respectively [
17]. Both patients had hemorrhagic infarcts, with massive bleeding at the core of the infarct. Both in vivo and ex-vivo T2W showed areas of low signal intensity within areas of high signal intensity that corresponded to hemorrhage and edema, respectively. Thus, although we have no direct proof of the presence of hemorrhage in our patients, we believe that these studies sufficiently show that hemorrhage and hemoglobin breakdown leads to T2W signal attenuation as documented in our study. Our results are roughly in line with the results from previous studies that used T2*(‘star’)-weighted gradient-echo techniques to visualize IMH [
10,
11]. Asanuma et al. found IMH in 9 of 24 (38%) patients with reperfused anterior MI [
10]. Patients with IMH had larger enzymatic infarct size, more Q-wave infarctions and less improvement in echocardiographic wall motion score. Ochiai et al. showed IMH in 13 of 39 (33%) patients with reperfused infarction, and also found an association between IMH, infarct severity and less improvement of ventriculographic ejection fraction [
11]. There are no studies comparing T2W spinecho imaging to T2*-weighted gradient-echo imaging for the assessment of IMH, and, at this point, it is not clear which is the optimal technique for its visualisation. Cardiac application of both techniques has been validated in a limited number of experimental and pathological studies [
9,
11,
18]. Although T2*-weighted gradient-echo imaging is very sensitive to the paramagnetic effects of the deoxyhemoglobin and methemoglobin, it requires relatively long echo times that may degrade image quality during cardiac imaging [
8]. T2W spinecho imaging has the advantage that it also depicts infarct related edema, which has been shown to correspond to the area at risk [
19,
20]. In line with a recent report by Friedrich et al., we found that mean (single slice) T2W infarct area was (approximately 70%) larger than DE infarct area [
20].